Responses of Steller Sea Lions (Eumetopias jubatus) to In-Air Blast Noise from Military Explosions

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The Steller sea lion (Eumetopias jubatus) is a species of conservation concern and is protected from anthropogenic disturbances by federal legislation in Canada and the United States. Although the breeding population has tripled since intensive culling ended ~40 y ago, conservation concerns persist due in part to the species’ vulnerability to anthropogenic factors, including noise. Published data on the nature and consequences of Steller sea lion responses to loud, impulsive noises such as explosions are sparse, yet useful where important haulouts are adjacent to such events. Herein, we document the short-term behavioural responses of Steller sea lions on a winter haulout complex to military explosions on southern Vancouver Island, Canada, over a period spanning 1997 to 2010. Blasting activities have been ongoing for over 70 y, involving ordnance disposal and on-land demolition training with high explosives-both of which disturb pinnipeds at nearby Race Rocks Ecological Reserve (RRER). Acoustic measurements confirmed that in-air noise reached levels capable of causing pinniped disturbance (i.e., > 109 dBF peak) but not injuries such as a permanent threshold shiftin hearing (i.e., < 149 dBF peak). Sea lions showed a significant increase in activity following blasting and were commonly displaced from haulouts. Within minutes of the disturbance, however, activity levels dropped sharply, and displaced animals usually began returning to haulouts. Activity levels on the day after blasting were similar to levels on days prior to blasting. General linear models showed no evidence (2 models) or no conclusive evidence (1 model) of an effect of blasting on sea lion abundance. Repeated exposure to in-air blast noise has short-term effects on Steller sea lions at RRER. We speculate that long-term effects on sea lions using RRER are unlikely-especially considering the increase in the peak numbers of Steller sea lions at RRER in recent decades while blasting has been ongoing. Key Words: Steller sea lion, Eumetopias jubatus, C4, disturbance, explosion, harassment, military, noise, ordnance, Race Rocks, Salish Sea, eastern stock.

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Publication: Aquatic Mammals
Author: Demarchi, Mike W
Date published: July 1, 2012
IntroductionA segment of the eastern stock of Steller sea lions (Eumetopias jubatus) occurs year-round in the marine waters of British Columbia (BC), Canada. There are four breeding areas in BC, and a number of others between Cape Suckling, Alaska, and California, and these sea lions also use numerous other locations along the coast as year-round or winter haulout sites (Fisheries and Oceans Canada, 2011). Hauling out at non-rookery sites confers a number of benefits to sea lions, including rest; decreased risk of predation by killer whales (Orcinus orca); and opportunities for nursing, grooming, and social interaction. Race Rocks Ecological Reserve (RRER) is one of at least 26 major haulout sites in BC that are used only by nonbreeding animals primarily during autumn and winter (Fisheries and Oceans Canada, 2011; LGL Limited, unpub. data); both sexes and all age-classes occur at RRER. Based on re-sight data from branded animals (Edgell & Demarchi, in press), RRER is used by Steller sea lions that breed in California, Oregon, and Alaska. The extent to which Steller sea lions from rookeries in BC use RRER is not known because no extensive branding or tagging studies have been conducted in BC. However, considering that the nearest rookeries in Canadian waters (i.e., Scott Islands) are closer than those in the U.S., we suspect that many of the Steller sea lions at RRER are from Canadian rookeries. Abundance of Steller sea lions in RRER varies by season and year, with counts ranging from 0 to 680 animals (Edgell & Demarchi, in press). However, the actual number of animals that use RRER during peak years is expected to be considerably greater as they use RRER as a temporary stopover while moving into and out of the Salish Sea. RRER is also frequented by California sea lions (Zalophus californianus), harbour seals (Phoca vitulina), and northern ele-phant seals (Mirounga angustirostris).The Steller sea lion is presently listed by the Committee on the Status of Endangered Wildlife in Canada (COSEWIC) as a species of Special Concern and is on Schedule 1 of the Canadian Species at Risk Act (SARA). It is the subject of a federal management plan that identifies acute noise disturbance as a management concern (Fisheries and Oceans Canada, 2011). In the U.S., the eastern stock of Steller sea lions, which extends from southeast Alaska to California, is listed as Threatened under the Endangered Species Act. Prior to garnering protection in Canadian waters under the Fisheries Act in 1970, and under the U.S. Marine Mammal Protection Act in 1972, Steller sea lions were extensively culled in an effort to reduce real or perceived conflicts with commercial fish-eries (Fisheries and Oceans Canada, 2011). Since then, the eastern stock has increased through 2002 (the year of the last range-wide survey) at a mean annual rate of 3.1% (Pitcher et al., 2007), and the number of breeding animals in Canadian waters has tripled (Fisheries and Oceans Canada, 2011).

At haulout sites, Steller sea lions are susceptible to disturbance and commonly enter the water when disturbed (e.g., Harestad, 1978; Lewis, 1987; Kucey, 2005; this study). The adaptive significance of this response is unclear given that overall mortality risk is likely greater in water (e.g., killer whale preda-tion, entanglement) than on land. However, such a response is appropriate in light of their vulnerabil-ity to harm by humans with rifles. Beyond RRER, sea lions are commonly shot for First Nations’ sub-sistence harvesting (e.g., as authorized under the Nisga’a Final Agreement and under Alaskan Native subsistence harvest agreements), animal control at aquaculture facilities (e.g., Hume, 2000; we note that in a recent review of human-caused mortality of Steller sea lions, Allen & Angliss 2012, indi-cated by way of a pers. comm. with P. Olesiuk that aquaculture facilities in BC have been forbidden from shooting Steller sea lions since 2004; how-ever, news reports of Steller sea lions being shot at aquaculture facilities do occur occasionally), and as perceived competitors with commercial fish-ing interests. Lewis (1987) reported that neonate Steller sea lion pups on a rookery were trampled to death by adult sea lions fleeing humans approach-ing by foot, but the extent of such mortality was low. Kucey (2005) documented numerous occa-sions of Steller sea lion disturbance, but no conse-quent injuries or mortalities were reported. Tershy et al. (1997) and Holcomb et al. (2009) concluded that human disturbance of California sea lions was short-term and localized.

The Marine Mammal Regulations under the Fisheries Act prohibit people from disturbing any marine mammal in Canadian waters unless authority has been granted by the federal government. Those regulations are not based on empirical evidence of harmful effects of disturbance but, rather, on the premise that interfering with the normal life functions of a marine mammal exposes it and its population to risks. It therefore follows that conservation interests can be served by managing risk exposure. However, if the putative disturbance has no negative implications for population conservation, or even if the population consequences are sustainable, restricting human activities such as military training or ecotourism for the sake of preventing disturbance could have negative social or economic consequences that might not be justified by the restrictions. That said, the use of best practices toward achieving environmental sustainability dictates that viable options to integrate human activities with the interests of marine mammal ecology should be identified and implemented whenever possible.

Canadian Forces Base (CFB) Esquimalt and Canadian Forces Ammunition Depot (CFAD) of the Canadian Department of National Defence (DND) oversee exercises and operations involving explosives in Marine Training and Exercise Area WQ at Rocky Point on southern Vancouver Island, BC. The Rocky Point property was selected and subsequently appropriated by the DND in 1955 as the site for the West Coast ammunition depot, thereby replacing the Colwood depot in Esquimalt Harbour (Mathews, 2004). The training that occurs at Rocky Point has been ongoing for over 70 y and includes defensive exercises, service battalion training, and demolitions training (Ferg, 1996). Such training is imperative for those members of the Canadian Forces that are engaged in both domestic and foreign operations. To this day, Rocky Point is still the largest terrestrial training area under the administration of the CFB Esquimalt and plays an integral role in supporting the DND’s activities both on land and at sea. In order to aid in maintaining the current level of operational capability of the Canadian Forces, a high tempo of training is carried out at Rocky Point year-round and will continue into the foreseeable future.

Military activities involving explosives are known to disturb Steller sea lions and other pinnipeds at nearby RRER, and the in-air audiogram of Steller sea lion (Muslow & Reichmuth, 2010) confirms that blast noise is audible to this species. Ferg (1996) identified information gaps in our understanding of the implications of military training for Steller sea lion ecology in RRER. Since then, pinniped monitoring has taken place intermittently in conjunction with DND activities. We selected the Steller sea lion as the focal species for this study because of the four species of pinniped that occur at RRER, it has the highest conservation status (listing) and has been observed to be the most responsive to acoustic disturbances. In support of this goal, the research objectives of this program were to document the responses of Steller sea lions to military explosions and to quantify the short-term effects on the use of RRER by those animals. Depending on the nature of the short-term effects, the potential for long-term effects, which are far more complicated to measure and detect, might be gauged.

Materials and Methods

Study Area

Marine Training and Exercise Area WQ is located on Rocky Point, southern Vancouver Island, BC (48° 19’12” N, 123° 33’13” W). Two ranges within WQ are used for ordnance-based demolitions training: (1) the Whirl Bay Underwater Demolition Range and (2) the Bentinck Island Demolition Range (Figure 1). The Bentinck Island Demolition Range is used for above-water beach-clearing and obstacle-creation exercises (e.g., metal cutting and the displacement and demolition of rocks and logs). The range is used for up to ~12 training courses per year, each spanning 1 to 4 d. With the exception of one or two night courses annually, all blasting occurs during daylight hours.

During the study period, demolitions (aka projects) at Bentinck Island comprised up to a maximum of four slabs of C4 plastique. C4 is a white, plastic high explosive made of RDX (Royal Demolition Explosive; aka cyclonite or hexogen; chemical name, trinitrotriazine) and an inert plastic binder. On a typical day, one to three projects are detonated in a run (or series) with ~30 s to 5 min or more between projects and ~15 to 120 min between two to four runs (i.e., 4 to 12 blasts in total). Some project locations have a direct line-of-sight to most of RRER, and others are separated to a modest degree by beach and island topography. The nearest haulout used by seals and sea lions in RRER is ~1.3 km from the blasting site at Bentinck Island.

Surplus ordnance is disposed of on an as-needed basis on the Christopher Point Ordnance Disposal Range, which has a line-of-sight to RRER (Figure 1). Up to 12 detonations can occur per day. Use of the range varies greatly among years, but it is typically used fewer than 25 d/y. The nearest haulout used by pinnipeds in RRER is ~2.0 km away from the detonation site at Christopher Point.

The pinniped study area comprised the exposed portion of RRER (Figure 1). RRER is a complex composed of one island (Great Race Rock: 1.48 ha; 48° 17’55” N, 123° 31’54” W) and a number of smaller rocky islets and reefs. To facilitate animal counts and account for the spatial separation of individual haulouts within the RRER complex, the pinniped study area was subdivided into 14 sub-areas (haulouts) that varied in size and extent of use by pinnipeds. Terrestrial vegetation occurs only on Great Race Rock and consists of grasses and small forbs of both native and Eurasian origin. Great Race Rock has a number of buildings and infrastructure, including an automated light station operated by the Canadian Coast Guard. RRER is in the Salish Sea near the eastern end of Juan de Fuca Strait and is in the Nanaimo Lowland Ecosection of the Eastern Vancouver Island Ecoregion of the Georgia Depression Ecoprovince (Demarchi et al., 1990). The climate of the study area is mild, being moderated by the Pacific Ocean. Tides are semidiurnal with strong diurnal inequality. Actual tide height ranges between -0.367 and 3.707 m (chart datum), and tidal flow through Race Passage can reach 13 km/h.

Acoustic Monitoring

In-air sound levels of blast noise reaching Great Race Rock were obtained using a Larson Davis System 824 logging sound level meter (SLM), equipped with a 0.64-cm free-field microphone and windscreen during 4 d in 2007. The SLM logged broadband sound levels at Great Race Rock during the blast noise trials. Pressure waveforms from the SLM microphone were digitally recorded at 48-kHz sampling rate with 24-bit resolution for subsequent spectral and waveform analysis. The microphone was oriented toward Bentinck Island in a line-of-sight and was mounted on a tripod at a height of 170 cm above ground level near the northern limit of Great Race Rock nearest Bentinck Island.

The recording system was calibrated at the start of each day using a Larson Davis CAL200 94/114 dB re 20 µPa sound calibrator. The microphone was located ~1,950 m from the demolition area which is ~200 m (11%) farther from Bentinck Island than the main Steller sea lion haulout in RRER (i.e., “middle” rock; see Figure 1). The following three sound pressure level (SPL) metrics are presented: (1) peak SPL (the maximum instantaneous pressure level over the pulse duration), (2) impulse time-weighted SPL (i.e., the rms [root mean square] pressure level computed using a 35 ms exponential time-weighted moving average); and (3) 1 s energy equivalent SPL (denoted Leq) (i.e., the maximum rms pressure level over a fixed 1 s time window encompassing the pulse). The flat-weighted 1 s Leq was numerically equal to the unweighted sound exposure level (SEL) for exposure to single blast events since the duration of the measured blast pulses was less than 1 s. Both flat-weighted (i.e., unweighted) and A-weighted SPLs are presented, in units of dBF and dBA, respectively, in order to facilitate comparison of the results of this work to other studies.

A parabolic-equation-based atmospheric sound propagation model (INPM) was used to estimate the noise footprint of Bentinck Island blast operations. The model accurately computes frequency dependent sound propagation, accounting for diffraction, air turbulence, and ground interaction. Ground elevation data for the modeling area were obtained in the form of standardized 3 arc s resolu-tion Digital Terrain Elevation Data (DTED) files. Atmospheric wind and temperature profiles were measured using a weather balloon probe launched from the CFB Esquimalt MetOc station (CWPF), located ~15 km northeast of RRER. A single balloon launch was performed between 0800 h and 1000 h local time on each day of noise measurements. Modeling was performed in standard 1/3-octave fre-quency bands from 6.3 to 630 Hz.

Sea Lion Monitoring

The study focused on demolitions conducted on Bentinck Island, but detonations on Christopher Point were occasionally monitored because of their potential to disturb pinnipeds. We did not conduct a thorough study of the underwater demolitions in Whirl Bay, though we know from previous work that the in-air noise levels of underwater explosions are greatly reduced compared to in-air noise levels of above-water detonations (LGL Limited, unpub. data, 1997 to 2010).

Observations of Steller sea lions on haulouts were made by two biologists using binoculars and a spotting scope from atop the lighthouse on Great Race Rock (Bushnell 8 × 40; 15 to 45 × 60; ~30 m above sea level; ~650 m to farthest haulout) intermittently from 1997 to 1998, 2002 to 2003, and 2007 to 2010. On several occasions in 2008 it was necessary to count sea lions on part of one haulout from the water during daily boat trips to and from RRER because animals had shifted to a previously unused part of the haulout that was not visible from the tower. Most observations occurred during the peak of sea lion abundance, September to January. For Bentinck Island, monitoring was conducted on days prior to blasting (Pre-Blast BI), during blasting (Blast BI), and following blasting (Post-Blast BI), though not all Bentinck Island monitoring was part of such a sequence. For Christopher Point, monitoring only took place on days when detonations occurred. Pre-Blast BI monitoring provided a measure of baseline conditions ≥ 1 d prior to demolition exercises or ordnance disposal. Post-Blast BI monitoring provided an indication of animal abundance and behaviour 1 d after blasting. From the light tower, we maintained radio or visual contact with military personnel regarding the blasting schedule. Blasts, as heard by the observers, were noted to the nearest second.

Morning (AM) and afternoon (PM) censuses of Steller sea lions in RRER (i.e., all haulouts) provided information about daily changes in the total number of animals using the study area. The morning census occurred prior to any blasting. With one exception, the afternoon census occurred after the last blast of the day. Only animals that were supported by terrestrial features (i.e., islands, islets, rocks, jetty, etc.) were counted because of the difficulties in seeing and counting animals in the water. Although some animals were hidden from view, in our opinion and based on our familiarity with the area (including views from the water during travel to and from the island), most (> 90%) hauled-out individuals were visible from the tower. Crowding also may have biased the estimates because some animals obscured our view of others-especially when they were resting in the prone position. Increased activity (e.g., heads up) sometimes resulted in a higher and more reliable sea lion count per a given haulout.

Scan sampling of Steller sea lions on specific haulouts (sub-areas) within RRER allowed us to evaluate differences in behaviour and haulout density pre- and post-disturbance. Whereas the twice-daily census tallied all animals in RRER, scan samples comprised animals on a subset of haulouts in RRER, and, as such, the reactions of all Steller sea lions in RRER to disturbance stimuli were not monitored. Haulouts monitored for scan sampling were selected and sampled in the morning (prior to any blasting) and had ≥ 10 animals present during the first sample. Those haulouts were then monitored throughout the remainder of the day. Behaviour was defined as active or inactive. An active animal was one with its head up, was moving about the haulout, or was engaged in social interaction as per Harestad (1978). Counts of Steller sea lions on sub-areas selected for daily monitoring prior to any blasting were usually made at ~30 to 60 min intervals during the observation period, plus additional counts were made immediately before and in the minutes following a run (or projects within a run if time between projects permitted). Post-blast counts were made soon after all animals entered the water or it was apparent to the observer that movement to the water had largely ceased. Two visible measures of disturbance were recorded: (1) the relative change in behaviour (i.e., activity level) and (2) the change in number of animals hauled out after a disturbance as compared with before the disturbance. The proportion of active animals (i.e., activity level) was calculated by dividing the number of active individuals by the total number in a given sub-area. Displacement from a given haulout was quantified by comparing sequential samples.

Environmental data were collected periodically throughout all monitoring days. These data were recorded at the start and end of each day (approximately concurrent with the AM and PM census events), and whenever weather changed notably. Environmental parameters included air temperature, wind direction and speed, Beaufort sea state, swell height, cloud cover, precipitation, and tidal height. Swell height was recorded as a categorical variable with four levels (none, low, medium, high). Precipitation was recorded as a categorical variable with five levels (none, fog, light rain, hard rain, snow). Wind data were obtained from Coast Guard instrumentation on the light tower. Hourly tide data were obtained from Fisheries and Oceans Canada for Victoria Harbour.

Activity Analysis

Activity data were imported to MS Excel and SYSTAT 12 for graphing and statistical analyses. Activity data (percentages) were arcsine transformed before analysis, and the homogeneity of variance was examined using Levene’s test. Activity data were analyzed using ANOVA and Tukey HSD tests. Activity data were averaged over the course of a day because daily averages were more appropriate for statistical testing than individual values obtained from repeated observations of the same animals on the same day. To account for potential biasing effects of proportions resulting from samples with few animals, in addition to testing all records involving ≥ 1 animal, we set an arbitrary minimum threshold of 10 or 50 animals, depending on the analysis.

Census Analysis

Census data from eight monitoring sessions comprising consecutive pre-blasting (1 d), blasting (1 to 4 d), and post-blasting (1 d) days were compared. In addition, census data were analyzed with general linear models (GLM) using R, Version 2.13.2. Three such analyses were conducted, each using different predictive parameters to examine the effect of blasting. In the first analysis, a continuous blast parameter called “Blast Number” was used. It was the number of blasts that occurred leading up to the associated census observation. For all AM censuses, the Blast Number was 0. For PM censuses, the Blast Number was the number of blasts that had occurred on the monitoring day prior to the census (PM Blast Number was 0 on non-blasting days). In the second analysis, two categorical blasting parameters were used: (1) “Blast-day” (yes/no) and (2) “Census” (AM/PM). For this analysis, a statistically significant interaction between these two parameters would indicate an effect of blasting (i.e., the AM/PM sea lion counts would be expected to vary on days when blasting occurred but not on non-blast days). In the third analysis, a categorical blasting parameter called “Day-type” was used. Day-type categories included “pre-blast days,” “blast days,” and “post-blast days.” Because data from only 5 d of blasting on Christopher Point were collected, they were excluded from all three analyses. The first two analyses included 144 censuses, recorded on 72 d (2/d) between 2002 and 2010 (not all environmental data were collected in 1997). Data for the third analysis were restricted to the PM censuses.

For all models, the number of sea lions hauled-out was the response variable. As is typical when the response variable is a count, the models were initially run with a Poisson error distribution (Crawley, 2007). Initial tests showed strong evidence of overdispersion (the residual deviance was much greater than the residual degrees of freedom), thus all subsequent models were run using an overdispersed Poisson error distribution (i.e., “quasi-Poisson”).

As a starting point for all three analyses, the models included the full suite of environmental variables as covariates. Some environmental variables were included “as measured,” including air temperature, Beaufort sea state, cloud cover, and tide height. Both swell height and precipitation were recorded with too much precision, and categories needed to be pooled for analysis. Swell height was collapsed to three categories (none, low, and medium-high), and precipitation was collapsed to two categories (yes and no). Wind was componentized into a “north-south wind speed” and an “east-west wind speed” for analysis. Componentization was done by taking the sine (or the cosine) of the recorded wind direction and multiplying it by wind speed.

For these analyses, fully factorial models could not be evaluated due to over-parameterization and limited degrees of freedom (e.g., 3,069 degrees of freedom would be required to evaluate a fully factorial form of the model in Analysis 1). It was therefore necessary to limit the “saturated” model to main effects and first-order interactions (Analysis 2 also included three-way interactions involving Blast-day and Census). Models were reduced in a stepwise progression by removing parameters one or a few at a time and evaluating the reduced model against the previous version. Reductions occurred in order of decreasing “significance,” starting with interactions before proceeding to the main effects. Main effects were not removed if they were involved in an interaction term that was retained in the model. F-tests were used for model comparison (since AIC could not be evaluated for models with overdispersed error distributions), and the reduced model was selected as the more parsimonious when no significant difference was observed. For each of the three analyses, a final model was selected. To test the significance of each model term, we fit models with and without the term and then compared the models using an F-test.

Results

Acoustic Monitoring

Acoustic measurements were obtained on Great Race Rocks during 31 detonations of C4 on Bentinck Island (Table 1). SPLs received at Great Race Rock were independent of charge size (r = 0.044, n = 31). Acoustic propagation modeling indicated that SPLs at those haulout areas in RRER that were closer to the demolition range (~1,300 to 1,750 m cf. 1,900 m) would be within ±3 dB of SPLs measured at Great Race Rock, depending primarily on prevailing wind conditions.

Sea Lion Activity

A total of 113 d of monitoring was conducted. No on-site night monitoring was conducted during this study, although a single blast at dusk (~2005 h) on 12 September 2008 was viewed remotely via a webcam. That blast caused sea lions to raise their heads, but none were observed moving to the water. Average activity levels were variable but tended to be greatest during Blast BI and lowest during Pre-Blast BI; activity levels during Post-Blast BI and Christopher Point detonations were intermediate (Table 2). A comparison of the mean daily activity levels among days when no range or one range was active indicated a significant difference (F = 7.818, df = 3, 76, p < 0.001 for samples involving ≥ 50 animals, and F = 8.078, df = 3, 95, p < 0.001 for samples involving ≥ 1 animal). Regardless of the minimum number of animals, pairwise compari-sons showed that the only significant difference was the result of greater activity levels on Blast BI days vs Pre-Blast BI days (p < 0.001).

Immediately following most blasts, activity levels spiked as animals raised their heads in response to the noise. None of our in-field observations or digital images suggested that the animals oriented toward the noise. Within minutes, activity levels of those animals remaining on the haulout dropped sharply and continued to diminish significantly with increasing time since the most recent blast (Figure 2; r = -0.322, p < 0.001, n = 1,087). By ~240 min since the most recent blast, average activity level approached the average level observed during Pre-Blast BI days (i.e., ~30%; Table 2 & Figure 2), but actual levels were variable.

Blasting was the most predictable cause of displacement, but Steller sea lions were observed to leave a haulout in response to approaching boats, swells washing over the haulout, pedestrians on Great Race Rock, and unknown factors. Departure from a haulout was greatest on those days when blasting occurred on Bentinck Island or Christopher Point, but notable decreases in numbers, including complete haulout abandonment, were also observed on days prior to and after blasting on Bentinck Island (Figure 3). Similarly, increases in the number of sea lions on a given haulout were observed, including on days when blasting occurred. The distribution of data > 0 for the Bentinck category of Figure 3 shows that animals displaced by blasts commonly returned to the haulout. Note, however, that these haulout-specific counts do not account for animals that were displaced but that hauled out elsewhere in RRER.

Sea Lion Census

Four analyses were performed on the census data, and none provided evidence of significant effects of blasting on the numbers of Steller sea lions hauled out in RRER.

Eight monitoring sessions comprised consecutive monitored days of Pre-Blast BI, Blast BI, and Post-Blast BI. Despite increases in activity levels and displacement from haulouts during blasting days, we observed both decreases and increases in the maximum count of any census during the day of Post-Blast BI monitoring as compared to the maximum count observed during the day of Pre-Blast BI monitoring or the first census on the morning of the first day of blasting (prior to any explosions) (Tables 3 & 4). Moreover, the highest counts (627 and 630) of the eight sessions were observed during the respective mornings of a Pre-Blast BI day and a Post-Blast BI day during a single session in October 2009 (Table 3).

For analysis GLM 1, the model examining the effects of Blast Number was reduced to its most parsimonious form (r2 = 0.16), including Beaufort sea state (p = 0.007), cloud cover (p < 0.001), air temperature (p = 0.006), and the cloud cover × air temperature interaction (p < 0.001). Models including Blast Number were not significantly better than those that excluded it, thus the simpler, reduced models were more parsimonious.

For analysis GLM 2, the model examining the effects of the Blast-day × Census interaction was reduced to its most parsimonious form (r2 = 0.23), including Blast-day (p = 0.006), swell height For analysis GLM 2, the model examining the effects of the Blast-day × Census interaction was reduced to its most parsimonious form (r2 = 0.23), including Blast-day (p = 0.006), swell height (p = 0.027), cloud cover (p = 0.002), Beaufort sea state (p > 0.05), air temperature (p = 0.049), and two interaction terms: Blast-day × Beaufort sea state (p = 0.002), and cloud cover × air temperature (p = 0.007). Models that included the Blast-day × Census interaction were not significantly better than those that excluded it, thus the simpler, reduced models were more parsimonious. Although the interaction term was of greatest interest for this analysis, the Blast-day term was nevertheless retained in the final model. Specifically, the number of Steller sea lions was significantly and negatively affected by sea state on blast days (regardless of whether the observations were made in the morning before the blasts or in the afternoon after the blasting) but not on non-blast days. Reconfirming that Census was not an important factor, there was no significant difference between the final model and one which was expanded to include Census and the Census × Blast-day × Beaufort sea state interaction (p = 0.490).

For analysis GLM 3, the model examining the effects of Day-type was reduced to its most parsimonious form (r2 = 0.15), including only swell height (p = 0.005). Models including Day-type were not significantly better than those that excluded it, thus the simpler, reduced models were more parsimonious.

Discussion

During monitoring spanning 1997 through 2010, explosions in Military Training Area WQ led to increased activity levels and caused Steller sea lions to move from haulouts to water in RRER. The explosions produced received sound levels in RRER that exceeded the threshold level for behavioural responses of pinnipeds to in-air noise of 109 dBF (peak) as proposed by Southall et al. (2007), but they were well below the level of 149 dBF (peak) proposed as a threshold for injury (i.e., permanent threshold shift[PTS] in hearing) by those same authors. Consequently, the direct impacts of military training are believed to have been mediated via a behavioural, and not a physiological, pathway-although non-auditory physiological responses (e.g., stress) cannot be ruled out. The first visible response by a sea lion to a blast was typically the change from a prone or other relaxed position to an alert, head-up pos-ture. Sea lions typically reacted to detonations on Bentinck Island or Christopher Point by quickly raising their heads and assuming an alert posture. In many instances, some or all of the animals then moved offthe haulout and into the water. Thereafter, activity levels of those animals that remained on the haulout diminished within min-utes of the disturbance as animals began returning to a prone position (Figure 2). Although the differ-ence was not statistically significant, mean activity levels did suggest that there were some residual effects of disturbance during the post-blast moni-toring day. If this was not a spurious observation, it could have been a result of ongoing recovery since blasting, increased sensitivity to other stimuli (e.g., weather, ecotour boats), or both.

There was no indication that blasting displaced a majority of sea lions from RRER. The maxi-mum counts observed the first day after blasting were sometimes higher and sometimes lower than during the first count made ahead of any blasting on those days when the Bentinck Island range was active. Models showed no adverse effect of blast-ing on sea lion census counts, except in conjunc-tion with higher sea states. However, this latter result was likely spurious because the same trend was observed for census counts made before blast-ing began on blast days. Other researchers have shown that pinnipeds leave haulouts in response to loud noises or other anthropogenic disturbances, but that numbers on haulouts returned to pre-dis-turbance levels within timeframes of several hours to several days (e.g., Bowles & Stewart, 1980; Stewart, 1982, 1993; Stewart et al., 1994; Tershy et al., 1997; Holst et al., 2005, 2011; Kucey, 2005; ManTech SRS Technologies [MSRS], 2008; Holcomb et al., 2009).

Steller sea lions are well adapted to the extremely harsh environmental conditions of the North Pacific, and severe marine weather can cause increased activity and haulout abandonment similar to the behavioural responses to explo-sions (e.g., MWD, pers. obs., 9 September 2011). Although one might speculate that being hauled out confers a measure of protection against preda-tion by killer whales, we only witnessed one pred-atory event during 113 d of monitoring between 1997 and 2010. However, the predominance of resident (i.e., fish-eating) as opposed to transient (i.e., mammal-eating) killer whales in the Salish Sea might, in part, explain this result.

Kucey (2005) documented that disturbance during scientific research (visiting haulout sites and branding animals or collecting scats) caused a significant short-term decline in Steller sea lion numbers at haulouts after the disturbance period. Sixty percent of disturbed sites in her study reached full recovery within ~4.3 d after the disturbance. Lewis (1987) noted that disturbance of Steller sea lions at a breeding site during post-pupping censuses caused an increase in activity and female territoriality and aggression, as well as changes in the numbers of animals hauling out after dis-turbance. Lewis also documented a decrease in numbers of sea lions in the disturbed area and an increase at a nearby undisturbed area.

Lewis (1987) documented a negligible amount of Steller sea lion pup mortality as a result of trampling following human-caused disturbance. As part of a pup census, biologists walking through a rookery purposefully drove non-pups into the water. Of 483 pup carcasses examined, at least two but up to three (< 1%) were believed to have resulted from trampling; the two deaths due to trampling accounted for 0.03% of pups born that year. RRER is not a Steller sea lion rookery; and by the time pups arrive in late summer and early autumn, they are highly mobile and not as susceptible to trampling by adults as are neonates. No pup injury or mortality at RRER as a result of trampling by conspecifics has been documented during hundreds of hours of observations of numerous disturbance events since 1997.

In the absence of a large sample of radio-tagged animals, one cannot conclusively determine what proportion of the local population might be tempo-rarily or permanently abandoning RRER follow-ing each disturbance. Similarly, in the absence of a large number of marked animals, it is not possi-ble to distinguish sea lions that return to a haulout after being displaced due to a blast from those returning from at-sea foraging or those migrat-ing individuals that arrive at the haulout after, and independent of, blasting activity. In spite of these limitations, the increases in the number of animals on haulouts that were commonly observed after a recovery period following a disturbance event were greater than increases observed during non-blasting days. This strongly suggests that recently displaced animals, and not newly arriv-ing migrants or animals returning from foraging trips, were returning to the haulouts. On a few occasions, we observed branded individuals leav-ing and returning to a haulout. Additionally, for those years when enough counts were conducted to reveal a seasonal peak in numbers, the number of Steller sea lions at RRER increased steadily (r2 = 0.672, p < 0.001, n = 17) from fewer than 10 ani-mals in 1965 (Bigg, 1988) to at least 680 in 2009 (Edgell & Demarchi, in press). That increase, at a time during which ordnance disposal and military training with high explosives occurred in Training Area WQ, provides further evidence that it is unlikely that military activities have caused any significant, long-term adverse effects on Steller sea lions using RRER. For greater certainty, by adverse effects we are referring to habitat exclusion, injury, or mortality. Considering the foregoing, it is not surprising that non-injurious acoustic stimuli would cause short-term behavioural effects persisting for no more than a few hours or a few days.

In conclusion, blasting in Marine Training and Exercise Area WQ causes short-term disturbance of Steller sea lions in RRER, and such disturbance is regulated under the Fisheries Act. However, the disturbance appears to be reversible and of a magnitude that is not believed to have caused significant adverse effects-at either a local scale or, by extension, a regional scale-for that segment of the eastern stock of Steller sea lions that occupies RRER. Despite this, the use of best practices dictates that options to mitigate the disturbance effects of blasting and other human activities be employed whenever practical. For example, seasonal blasting windows could be highly effective to the extent that overlap in blasting schedules and periods of peak sea lion abundance is reduced.

Acknowledgments

This study was funded by the Canadian Department of National Defence, Formation Safety and Environment, Canadian Forces Base Esquimalt and by LGL Limited. G. Smith, D. Freeman, D. Smith, and T. Cornforth (DND, Formation Safety and Environment) provided important project support. R. Price, A. Smith, R. Sharp, A. Steele, and A. Ransome-Hodges (Public Works and Government Services Canada) coordinated project administration. Dr. S. R. Johnson, then of LGL Limited, provided invaluable assistance initiating the study. We acknowledge the support of other DND personnel over the years and that of staffwith the Department of Fisheries and Oceans, the Canadian Coast Guard, BC Ministry of Environment, and Lester B. Pearson United World College of the Pacific. This research was done in accordance with ecological reserve permits issued by the Province of BC. Two anonymous reviewers kindly provided beneficial comments on an earlier version of this manuscript.

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Bigg, M. A. (1988). Status of the northern sea lion, Eumetopias jubatus, in Canada. Canadian Field-Naturalist, 102(2), 315-336.

Bowles, A. E., & Stewart, B. S. (1980). Disturbances to the pinnipeds and birds of San Miguel Island, 1979-1980. In J. R. Jehl, Jr. & C. F. Cooper (Eds.), Potential effects of space shuttle sonic booms on the biota and geology of the California Channel Islands: Research reports (pp. 99-137). San Diego: Center for Marine Studies, San Diego State University, and Hubbs/Sea World Research Institute for U.S. Air Force.

Crawley, M. J. (2007). The R book. Sussex, UK: John Wiley & Sons. http://dx.doi.org/10.1002/9780470515075

Demarchi, D. A., Marsh, R. D., Harcombe, A. P., & Lea, E. C. (1990). The environment. In R. W. Campbell, N. K. Dawe, I. McTaggart-Cowan, J. M. Cooper, G. W. Kaiser, & M. C. E. McNall (Eds.), The birds of British Columbia, Volume 1 (pp. 55-144). Victoria, BC: Royal British Columbia Museum.

Edgell, T. C., & Demarchi, M. W. (in press). Understanding forty-five years of California and Steller sea lion use of a major winter haulout in the Salish Sea. Marine Ecology Progress Series.

Ferg, V. D. (1996). Training Area Planning System (TAPS) Phase II: An assessment of military training at CFB Esquimalt. Victoria, BC: CFB Esquimalt, Department of National Defence.

Fisheries and Oceans Canada. (2011). Management plan for the Steller sea lion (Eumetopias jubatus) in Canada (Species at Risk Act Management Plan Series). Ottawa, ON: Fisheries and Oceans Canada.

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Holst, M., Lawson, J. W., Richardson, W. J., Schwartz, S. J., & Smith, G. (2005). Pinniped responses during Navy missile launches at San Nicolas Island, California. In D. K. Garcelon & C. A. Schwemm (Eds.), Proceedings of the Sixth California Islands Symposium, Ventura, CA, Dec. 2003 (National Park Service Technical Publication CHIS-05-01, pp. 477-484). Arcata, CA: Institute of Wildlife Studies.

Holst, M., Greene, C. R., Jr., Richardson, W. J., McDonald, T. L., Bay, K., Schwartz, S. K., & Smith, G. (2011). Responses of pinnipeds to Navy missile launches at San Nicolas Island, California. Aquatic Mammals, 37(2), 139-150. http://dx.doi.org/10.1578/AM.37.2.2011.139

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Kucey, L. (2005). Human disturbance and the hauling out behavior of Steller sea lions (Eumetopias jubatus) (Master’s thesis). University of British Columbia, Vancouver, Canada.

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ManTech SRS Technologies (MSRS). (2008). Final report for the 5-year programmatic permit for taking marine mammals incidental to space vehicle and test flight activities from Vandenberg Air Force Base, California, 6 February 2004 through 17 October 2008. Lompoc, CA: MSRS for the U.S. Air Force.

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Pitcher, K. W., Olesiuk, P. F., Brown, R. F., Lowry, M. S., Jeffries, S. J., Sease, J. L., . . . Lowry L. F. (2007). Status and trends in abundance and distribution of the east-ern Steller sea lion (Eumetopias jubatus) population. Fishery Bulletin, 105, 102-115.

Southall, B. L., Bowles, A. E., Ellison, W. T., Finneran, J. J., Gentry, R. L., Greene, C. R., Jr., . . . Tyack, P. L. (2007). Marine mammal noise exposure criteria: Initial scientific recommendations. Aquatic Mammals, 33(4), 411-522. http://dx.doi.org/10.1578/AM.33.4.2007.411

Stewart, B. S. (1982). Behavioral response of northern elephant seals (Mirounga angustirostris) and California sea lions (Zalophus californianus) on San Nicolas Island to loud impulse noise. In Studies on the pinnipeds of the southern California Channel Islands, 1980-1981 (HSWRI Technical Report 82-137, pp. 4-35). San Diego: Hubbs/Sea World Research Institute for U.S. Air Force Space & Missile Systems Organization and the National Marine Fisheries Service, Washington, DC.

Stewart, B. S. (1993). Behavioral and hearing responses of pinnipeds to rocket launch noise and sonic boom. The Journal of the Acoustical Society of America, 94(3), 1828. http://dx.doi.org/10.1121/1.407787

Stewart, B. S., Francine, J. K., & Thorson, P. H. (1994). Taurus launch at Vandenberg Air Force Base, 13 March 1994; sound levels and behavioral responses of harbor seals (Phoca vitulina richardsi) at Purisma Point and Rocky Point (HSWRI Technical Report 94-252). San Diego: Hubbs-Sea World Research Institute for U.S. Air Force, SMC/CEW, Vandenberg Air Force Base, CA.

Tershy, B. R., Breese, D., & Croll, D. A. (1997). Human perturbations and conservation strategies for San Pedro Mártir Island, Isla del Golfo de California Reserve, México. Environmental Conservation, 24(3), 261-270. http://dx.doi.org/10.1017/S0376892997000349

Author affiliation:

Mike W. Demarchi,1 Meike Holst,1 Dave Robichaud,1

Mike Waters,2 and Alexander O. MacGillivray3

1 LGL Limited, environmental research associates, 9768 Second Street, Sidney, BC V8L 3Y8, Canada

E-mail: demarchi@lgl.com

2 Formation Safety and Environment, Building 199D, Room 302, Canadian Forces Base Esquimalt,

PO Box 17000 STN Forces, Victoria, BC V9A 7N2, Canada

3 JASCO Applied Sciences, Suite 2101, 4464 Markham Street, Victoria, BC V8Z 7X8, Canad

Stylaster parageus columbiensis- Lindner & Cairns in Cairns & Lindner, 2011

Record in the Smithsonian Institute, from : http://collections.si.edu/search/record/nmnhinvertebratezoology_910698?q=set_name:%22Invertebrate+Zoology%22

Stylaster parageus columbiensis Lindner & Cairns  (**in Cairns & Lindner, 2011)

Paratype for Stylaster parageus columbiensis Lindner & Cairns in Cairns & Lindner, 2011
Catalog Number: USNM 1096625
Collection: Smithsonian Institution, National Museum of Natural History, Department of Invertebrate Zoology

Microhabitat Description:
shallow water
Collector:
Dr. Alberto Lindner
Ocean/Sea/Gulf:
North Pacific Ocean
Preparation: Dry
  • Sex: male
  • Type Status: Paratype
Place:
Strait of Juan de Fuca, Race Rocks near Sooke Community, British Columbia, Canada, North Pacific Ocean
Collection Date:
Jul 2002
Common name:
Hydrozoans
Taxonomy:
Animalia ,
Cnidaria ,
Hydrozoa,
Anthoathecatae
Stylasteridae
Published Name:
Stylaster parageus columbiensis Lindner & Cairns in Cairns & Lindner, 2011
Stylaster campylecus parageus (Fisher, 1938)
Stylaster sp.
Stylaster parageus (Fisher, 1938)
USNM Number:
1096625
Specimen Count:
1
Site Number:
AL 470
Record Last Modified:
17 Jul 2013
See more items in:
Invertebrate Zoology
Data Source:
NMNH – Invertebrate Zoology Dept.
Visitor Tag(s):
**Paratype: Cairns, S. D. & Lindner, A. 2011. A Revision of the Stylasteridae (Cnidaria, Hydrozoa, Filifera) from Alaska and Adjacent Waters. Zookeys. 158: 1-88.

See the entry of the Race Rocks Taxonomy

Tidal Current Energy Experiment Comes to an End.

September 17, 2011: Clean Current Staff and diving contractors return to Race Rocks to remove the generator for the last time. The generator returns to Vancouver for a final analysis of structural details after exposure in the ocean over the last three years . After cleaning,  it is to be sent to the Museum of Science and Technology in Ottawa, since it was the first ocean tidal generator to be built and deployed in Canada.

“In conclusion: The Tidal Current Generator operation over the past six years has been an interesting experiment and a good demonstration of the potential power from tidal energy.  The added value to the availability of energy for Race Rocks  was however very disappointing.

The main value to the Race Rocks program has been in the infrastructure that has been developed and installed and the potential for further research. The provision now of most of the energy needs by solar power was only made possible by the large bank of storage batteries provided by the project, the island energy building electrical infrastructure and the partnership with the BC Ministry of Mines and energy which were instrumental in providing the initial solar panels.  Installation of further solar panels and upgrades by Lester Pearson College UWC has helped to ensure energy sustainability for Race Rocks.

–Garry Fletcher

 

Race Rocks (XwaYeN) Proposed Marine Protected Area Ecosystem Overview and Assessment Report

Correct citation for this publication: Backe, N., S. Davies, K. Conley, G. Kosmider, G. Rasmussen, H. Ibey and K. Ladell.2011. Race rocks (XwaYeN) proposed marine protected area ecosystem overview and assessment report. Can. Manuscr. Rep. Fish. Aquat. Sci. 2949: ii + 30
Executive Summary
Background
Race Rocks (XwaYeN), located 17 km southwest of Victoria in the Strait of Juan de Fuca, consists of nine islets, including the large main island, Great Race. Named for its strong tidal currents and rocky reefs, the waters surrounding Race Rocks (XwaYeN) are a showcase for Pacific marine life. This marine life is the result of oceanographic conditions supplying the Race Rocks (XwaYeN) area with a generous stream of nutrients and high levels of dissolved oxygen. These factors contribute to the creation of an ecosystem of high biodiversity and biological productivity.In 1980, the province of British Columbia, under the authority of the provincial Ecological Reserves Act , established the Race Rocks Ecological Reserve. This provided protection of the terrestrial natural and cultural heritage values (nine islets) and of the ocean seabed (to the 20 fathoms/36.6 meter contour line). Ocean dumping, dredging and the extraction of non-renewable resources are not permitted within the boundaries of the Ecological Reserve. However, the Ecological Reserve cannot provide for the conservation and protection of the water column or for the living resources inhabiting the coastal waters surrounding Race Rocks (Xwa YeN) as these resources are under the jurisdiction of Fisheries and Oceans Canada (DFO). The federal government, through the authority of theOceans Act (1997), has established an Oceans Strategy, based on the principles of sustainable development, integrated management and the precautionary approach. Part II of the Oceans Act also provides authority for the development of tools nece ssary to carry out the Oceans Strategy, tools such as the establishment of Marine Protecte d Areas (MPA). This federal authority will complement the previously established protection to the area as an Ecological Reserve, by affording protection and conservation measures to the living marine resources. Under Section 35 of the Oceans Act, the Governor in Council is authorized to designate, by regulation, Marine Protected Areas (MPA) for any of the following reasons:

  • (a) the conservation and protection of commercial and non-commercial fishery resources, including marine mammals and their habitats;
  • (b) the conservation and protection of endangered or threatened species and their habitats;
  • (c) the conservation and protection of unique habitats;
  • (d) the conservation and protection of marine areas of high biodiversity or biological productivity; and
  • (e) the conservation and protection of any other marine resource or habitat as is necessary to fulfill the mandate of the Minister of Fisheries and Oceans.

In 1998, the Minister of Fisheries and Oceans announced Race Rocks (XwaYeN) as one of four pilot Marine Protected Area (MPA) initiatives on Canada’s Pacific Coast. Race Rocks (XwaYeN) meets the criteria set out in paragraphs 35(1) (a), (b) and (d) above. Establishing a MPA within the Race Rocks (XwaYeN) area will provide for a more comprehensive level of conservation and protection for the ecosystem than can be achieved by an Ecological Reserve on its own. Designating a MPA within the area encompassing the Ecological Reserve will facilitate the integration of conservation, protection and management initiatives under the respective authorities of the two governments.

physical and biological systems of Race Rocks (XwaYeN) was completed by Wright and Pringle (2001). The 2001 report provides an extensive ecological overview describing the geological, physical oceanographic and biological components of
Race Rocks (XwaYeN) and the surrounding waters of the Strait of Juan de Fuca at the time. Natural history observations and some traditional knowledge were also included. The following report is a brief update to summarize new information that has been collected in the Race Rocks (XwaYeN) area since that time and describe any changes
to trends in species distributions and oceanographic conditions. This work is meant to supplement the existing ecological overview (Wright and Pringle 2001).

See the full 32 page PDF  Ecosystem overview2011

Race Rocks Mean Monthly Sea Temperature 1921-present,

Seawater Temperature: Race Rocks
Decade Comparisons:Sea Surface Temperature at Race Rocks-
 

Year Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
1921 7.1 7.3 7.7 8.5 9.5 10.3 10.5 10.3 9.8 9.1 8.2
1922 6.4 6.1 6.6 7.5 8.3 9.5 10.5 10.3 10.2 9.3 8.4 7.1
1923 7.1 6.4 6.7 7.6 8.6 9.3 10.3 10.5 10.6 9.6 8.7 7.9
1924 7.1 7.3 7.7 7.9 9 9.8 10.5 10.3 10.2 9.2 8.8 7.3
1925 6.6 6.9 7.3 8 9.2 10.1 11.1 10.8 10.2 9.2 8.3 8.2
1926 7.8 8 8.6 9.2 10.1 10.7 11.1 10.9 10.5 9.8 9.1 8.5
1927 7.6 7.4 7.8 8 8.8 9.8 10.5 10.9 10.3 9.7 8.6 7.6
1928 6.9 7.3 7.8 8.6 9.7 10.2 10.8 10.9 10.3 9.2 8.6 7.9
1929 7.1 6.3 7.1 7.8 9 9.8 10.8 10.8 10.7 9.8 8.8 7.8
1930 6.5 6.6 7.1 8.2 9.3 10 10.6 10.8 10.6 9.4 8.6 8
1931 7.8 7.8 8.2 8.8 9.9 10.6 11.5 11.1 10.7 9.6 8.6 7.7
1932 7.1 6.8 7.3 8.2 9.3 10.4 10.8 10.9 10.7 9.6 8.9 7.7
1933 7.1 6.7 7.1 8 9.1 10.2 10.5 11.5 10.1 9.6 8.6 7.7
1934 7.8 7.9 8.3 9.2 10 10.8 10.9 11.6 10.7 9.7 9.2 8.4
1935 7.2 7.2 7.5 7.8 9.2 10.1 10.5 10.5 10.7 9.7 8.2 8.1
1936 7.9 6.7 7 7.8 9.3 10.4 11.3 11.3 10.5 10.1 8.6 7.9
1937 6.6 6.4 7.7 8.7 9.9 10.9 11.7 11.5 10.9 9.9 8.5 8.1
1938 7.4 7.2 8.1 9.4 10.6 12.3 12.7 11.9 11 9.9 8.6 7.5
1939 7.4 6.6 7.1 8.6 10.3 11.4 12.2 11.1 11.4 9.7 8.5
1940 7.9 8.2 9 10 11.4 11.6
1941 10 10.5 11.2 11 10.6 9.9 9 8.5
1942 7.9 7.9 7.8 8.5 9.6 9.8 10.5 11 10.3 9.5 8.4 7.9
1943 6.8 6.7 7.1 8.2 8.8 10 10.3 10.6 10.3 9.6 9 8.1
1944 7.7 7.5 7.3 8 9.2 10.5 11 10.9 10.5 9.6 9.2 8.1
1945 7.8 7.7 7.6 8 8.8 9.8 10.1 10.5 10 9.5 8.1 8.1
1946 7.7 7.3 7.7 8.1 9.4 10.2 10.7 10.8 10.3 9.4 8.1 7.7
1947 7.1 7 7.7 8.4 9.5 10.4 10.6 10.9 10.5 9.9 9.1 7.9
1948 7.5 6.9 7.2 7.9 9 10.2 10.8 10.7 10.4 9.5 8.2 7
1949 6.1 6.1 6.9 8.3 9.4 10.1 10.3 10.2 10.5 9.5 8.7 7.8
1950 6.2 5.8 6.6 7.7 8.7 9.4 10.1 10.4 10.3 9.3 8.5 8
1951 7.5 6.9 6.7 8.1 9.2 10.2 10.4 11.1 10.9 9.5 8.5 7.7
1952 6.9 7.1 7.6 8.2 9 9.6 10.4 10.5 10.2 9.8 8.6 7.9
1953 7.8 7.9 7.6 8.1 9.3 9.8 10.6 11 10.6 9.9 9.3 8.5
1954 7.1 7.3 7.5 7.9 8.7 9.3 9.9 10 10 9.4 9.1 8.4
1955 7.5 7.1 6.7 7.5 8.4 9.3 9.8 10.2 10 8.9 7.5 6.6
1956 6.7 6.4 6.3 7.6 8.7 9.6 10.2 10.4 10.1 9.2 8.1 7.1
1957 6.3 6.2 7.2 8.1 9.3 10 10.3 10.5 10.5 9.8 8.8 8.3
1958 8 8.3 8.6 9.3 10.3 10.7 11.5 11.5 11 9.9 8.7 8.1
1959 7.6 7.4 7.9 9.1 9.7 10.4 11.3 11 10.4 9.7 8.3 7.8
1960 7.1 7.5 7.5 8.6 9.6 10.3 11.4 10.8 10.1 9.5 8.6 7.9
1961 7.9 8.2 8.4 8.8 9.4 10.3 10.9 11.3 10.6 9.4 8.2 7.5
1962 7.2 7.3 7.3 8.4 9.3 10 10.4 10.5 10.5 10 9.3 8.7
1963 7.5 7.5 7.8 8.5 9.6 10.2 10.5 10.8 10.6 10.3 9.9 8.7
1964 8.2 7.9 7.7 8.2 8.8 9.6 10.3 10.5 10 9.4 8.3 7.4
1965 6.9 7.1 7.2 8 8.8 9.8 10 10.2 10.3 9.7 9.2 8.5
1966 7.7 7.6 7.7 8.5 9 9.1 99.9 10.7 10.1 9.5 8.7 8.6
1967 7.9 7.7 7.6 8.1 8.9 9.6 10.3 10.5 10.5 9.7 9.1 8
1968 7.3 7.3 8 8.3 8.7 9.5 10.2 10.2 10.4 9.3 8.8 7.8
1969 6.5 6.3 7.2 8.1 9.1 10.2 10.4 10.5 9.8 9.2 8.7 8.1
1970 7.5 7.7 7.9 8 8.7 9.6 10.2 10.2 10 9 8.3 7.5
1971 7 6.9 6.7 7.5 8.5 9.1 10 10.6 10.4 9.3 8.3 7.3
1972 6.4 6.2 6.9 7.6 8.8 9.5 10.5 10.6 10.2 9.1 8.4 7.3
1973 7 7.2 7.9 8.4 8.6 9.2 10.1 10.3 10 9.2 8.2 8
1974 7.2 7.2 7.3 8.1 8.5 9.7 10 10.9 10.6 9.7 8.6 8.2
1975 7.3 6.8 7.2 7.7 8.7 9.4 10.2 10.4 10.4 9.6 9.2 7.8
1976 7.2 7 7 7.8 8.7 9.3 10.1 10.1 10 9.4 8.6 8.1
1977 7.6 7.9 8 8.3 8.8 9.7 9.9 10.8 10.3 9.2 8.6 7.9
1978 7.6 7.9 8.3 8.9 9.4 10.3 10.4 10.9 10.5 9.8 8.2 7.3
1979 6.5 6.9 7.5 8.3 9.5 10 10.8 10.7 10.5 9.8 9 8.6
1980 7.7 7.6 7.9 8.6 9.5 9.5 10.6 10.9 10.5 9.9 9.2 8.6
1981 8.3 8.3 8.8 9.2 9.4 9.9 10.3 10.5 10.2 9.7 9.3 8.5
1982 7.2 7.5 8 8.8 9.9 10.7 11.4 11.8 11.4 10.3 8.8 8.3
1983 8.6 8.6 9.3 10 10.6 11.3 11.7 12.4 11.4 10.3 9.5 7.7
1984 7.5 7.8 8.4 9 9.7 10.3 11.4 11.6 10.6 9.7 8.5 6.9
1985 6.8 6.8 7.2 8.2 9.6 10.6 11.5 11.6 10.8 9.6 6.8 6.4
1986 7 6.6 8 8.4 9.4 11 10.9 11.8 10.8 9.8 8.4 7.8
1987 7.6 7.9 8.3 8.9 9.8 10.6 11.1 11.5 11.1 10 9 8.2
1988 7.4 7.5 7.5 8.6 9.6 10.4 11 11.4 10.6 9.6 8.7 7.9
1989 7 5.8 6.8 8.2 9.5 10.7 11.3 11.2 11 9.9 8.9 8.2
1990 8.1 7.7 8.2 9 9.9 10.8 11.8 12.1 12.1 10.7 9.9 8.2
1991 7.1 7.7 7.9 8.4 9.7 9.7 10.8 11 11.2 10.1 8.9 8.3
1992 7.9 8.1 9.5 9.5 10.2 10.7 11.1 11.4 11 10 9.1 7.8
1993 6.7 6.7 7.6 8.6 9.7 10.8 11 11.2 11 10.1 8.5 7.9
1994 8 7.4 8.6 9.3 10.1 10.6 11.6 11.5 11.3 10.7 9.3 8.4
1995 8.2 8.6 8.8 9.2 10.2 11.2 11.8 11.5 11.3 10.2 9.4 8.9
1996 8.2 7.8 8.4 9.2 10 10.4 11.5 11.5 10.5 9.9 8.7 7.6
1997 7.7 7.9 8.1 9 10.3 10.9 11.7 12.2 11.6 11.3 9.9 9.3
1998 8.7 9.2 9.7 9.9 10.4 11.4 11.7 12.3 12.1 10.7 9.8 9
1999 8 7.8 8.1 8.9 9.5 10.4 11.1 11.5 11.9 10.1 9 8.5
2000 7.5 7.7 8.1 9.1 10 11.1 11.3 11.7 11.4 10.3 9 8
2001 7.9 7.7 8.1 8.7 9.7 10.6 11.3 11.4 11.4 10.2 9.2 8.3
2002 8.1 7.9 7.7 8.7 9.4 10.5 11,2 11.7 11.3 10.0 9.0 8.8
2003 8.8 8.5 8.7 9.2 9.9 10.9 11.3 11.4 11.4 10.9 9.0 8.5
2004 7.8 7.9 8.3 9.1 10.4 11.0 11.8 11.9 11.2 10.6 9.4 8.6
2005 7.7 8.0 8.8 9.4 10.7 11.2 11.6 12.1 11.5 10.4 9.5 8.3
2006 8.61 8.49 8.41 8.75 10.08 10.86 11.66 12.09 11.49 10.55 9.29 8.5
2007 7.8 7.9 7.9 9.0 10.0 10.2 11.2 11.6 11.0 10.0 9.0 8.0
2008 7.46 7.33 7.68 8.06 9.36 9.77 10.84 11.30 11.16 10.14 9.39 7.87
2009 7.29 7.20 7.5 8.4 9.54 10.4 11.4 11.74 11.8 10.5 9.0 7.0
2010 8.11 8.68 9.12 8.96 9.54 10.36 11.16 11.93 11.08 10.37 8.98 8.5
2011 7.8
2012
2013
2014
2016
2017
2018
2019
2020
2021
2022
2023

 

Note, The blanks for the years 1940-41 are due to the Second World War. Apparently during that time, data was not collected by a lightkeeper.

Original data was sent by the Lightkeepers and now by the Marine Protected Area Guardian of Race Rocks to the Institute of Ocean Sciences where it is compiled and displayed at

http://www.pac.dfo-mpo.gc.ca/science/oceans/data-donnees/lighthouses-phares/index-eng.htm

Decade Average GraphDecade analysis by G. Fletcher.. NOTE probable evidence of climate change

 

Pseudocnus curatus: Black brooding sea cucumber–The Race Rocks Taxonomy

 

 

by Ryan Murphy, April, 2010 See Ryan’s underwater set on Flickr with a range of invertebrates:

In the early 1980’s while doing subtidal surveys, we discovered a major concentration of the small subtidal sea cucumber Pseudocnus curatus ( formerly Cucumaria pseudocnus) living in high density off the West side of Great Race Rocks. On April16, 2004, six divers, Ramiro, Mael, Mike, Carmen, Aven and Chris were able to do a preliminary survey of the area and have produced the results shown here.
To do the survey, they ran out a reel tape measure from shore to 75 meters in a bearing of 255 degrees magnetic from peg number 7- a permanent reference peg on the very South West corner of the Island. This took them into water that is 8 to 10 meters in depth.
We are uncertain as to why this organism concentrate here in these numbers, and this also happens at other locations such as Beecher bay 3 km to the West. This is the only area we find them in at Race Rocks.
Also included in this file are the raw data values from the divers. One may clip and paste these into an EXCEL program in order to do alternate analysis.

This species is distinguished from Cucumaria pseudocurata which lives up in the mussel beds by having 10 tentacles instead of 8. It is s found in great abundance on the surface of boulders at a depth of 10 meters 60 meters offshore of the south west tip of Great Race Rock ( peg7) Counts of up to 1000 per square meter have been estimated. It can also be found intertidally among the mussel beds on the Western side of the main island.

The following count done by students of the diving activity gives an idea of how dense this species is in one location at Race Rocks. Recently Ryan Murphy found another population of this density on the Eastside  of Great Race Rock.
The book Sea Cucumbers of British Columbia, Southeast Alaska, and Puget Sound by Phil Lambert is the best source for identification of most of the 45 species of local sea cucumbers. In it he notes that the habitat of Pseudocnus curatus “in the Juan de Fuca Strait tends to be shallow subtidal in areas where the tidal currents are strong….. They nestle together in large aggregations on open rocky surfaces …..and….. are eaten by many species of sea stars……although their body wall is toxic to some fish predators providing a strong defense mechanism.”

See also Taxing Problems by Philip Lambert – Now Curator Emeritus of Invertebrates, Royal BC Museum for a description of the difficulty in classification and the need to classify by the skin ossicles.
Google Pseudocnus curatus for a link to the page describing this species..

Pseudocnus curatus Is similar to another species, Cucumaria pseudocurata which is found more shallow in the intertidal zone at Race Rocks. Both species average 1.5 to 3cm in length. C. pseudocurata has 5 bands of tube feet in single or zig zag rows. As a rule there are 8 equal sized tentacles. P.curatus on the other hand has 10 equal sized tentacles. and tube feet scattered on the Dorsal side. At Race Rocks, it lives in the subtidal zone at 8 to 10 meters in depth.

Domain Eukarya
Kingdom Animalia
Phylum Echinodermata
Sub-Phylum Eleutherozoa
Class Holothuroidea
Subclass Dendrochirotacea
Order Dendrochirotida
Family Cucumariidae
Genus Pseudocnus
Species curatus, (Lambert,1997?)
Common Name: Black brooding sea cucumber

POPULATION DISTRIBUTION at RACE ROCKS

In the early 1980’s while doing subtidal surveys, we discovered a major concentration of the small subtidal sea cucumber Pseudocnus curatus ( formerly Cucumaria pseudocnus) living in high density off the West side of Great Race Rocks. On April16, 2004, six divers, Ramiro, Mael, Mike, Carmen, Aven and Chris were able to do a preliminary survey of the area and have produced the results shown here.
To do the survey, they ran out a reel tape measure from shore to 75 meters in a bearing of 255 degrees magnetic from peg number 7- a permanent reference peg on the very South West corner of the Island. This took them into water that is 8 to 10 meters in depth.
We are uncertain as to why this organism concentrate here in these numbers, and this also happens at other locations such as Beecher bay 3 km to the West. This is the only area we find them in at Race Rocks.
Also included in this file are the raw data values from the divers. One may clip and paste these into an EXCEL program in order to do alternate analysis.

Raw Data from 0.125 meter quadrats Ramiro and Mike and Av Carmen and Chris
meters from the shore 40
41
42 0
43
44
45
46 0
47 1
48 7
49 20
50 8
51
52 9
53
54 3
55
56
57 2
58 14
59
60
61
62 20
63
64 20
65 1
66 16 1
67 8
68 25
69 2
70 19 13
71 29
72 19
73 31
74 0

 

Other Members of the Phylum Echinodermata at Race Rocks 
taxonomyiconReturn to the Race Rocks Taxonomy
and Image File
pearsonlogo2_f2The Race Rocks taxonomy is a collaborative venture originally started with the Biology and Environmental Systems students of Lester Pearson College UWC. It now also has contributions added by Faculty, Staff, Volunteers and Observers on the remote control webcams.

Garry Fletcher

Wind Sentinnel Research

The Wind Sentinnel deployed at Race Rocks on October 18, 2009
-Estimated duration is Oct. 16 – Nov. 16 (logistics/weather dependant)
-Buoy Deployment Location – Lat: 48° 17.606’N    Long: 123° 32.370’W
-Communications – Buoy: Cellular phone
-Communications – land station: Race Rocks LAN wired Ethernet connection
.AXYSWindSentinelWe will be able to benefit by adding the information collected to the knowledge base for the reserve. It will also be useful for planning for future sustainable energy applications.

In October, 2009, Lester Pearson College had an opportunity to participate in an offshore wind assessment test by AXYS Technologies Inc. in the Strait of Juan de Fuca .See video of test in Juan de Fuca off Race Rocks
Sidney firm deploys world’s first wind buoy :
Times Colonist,October 28, 2009
Great Race Rocks was used to host the land station for an offshore buoy which is designed to record  wind speed and direction data profiles up to 200 meters height. It is anchored outside of the Race Rocks Ecological Reserve in the Strait of Juan de Fuca. Data from the buoy is relayed automatically every 10 minutes by cell phone to the instrument trailer on land and is transmitted to the internet through our LAN on Race Rocks.

See the Link below to this brochure pdf with more specifications

 

 

Link for more specifications AXYSWindSentinel

We will be able to benefit by adding the information collected to the knowledge base for the reserve. It will also be useful for planning for future sustainable energy applications

Our current wind measurements done by the Davis weather instrument we have installed on the ground level, often show at least a 10 km/h difference in wind velocity when compared with the Environment Canada data from the top of the tower at 36 metres. A set of data with projections to 200 metres will provide an excellent profile for comparisons.

See this sample file on Analyzing the data as an exercise
To access the Live Streaming Data from the instrument AXYS Technologies has provided the fiollowing link:http://data.axystechnologies.com/AXYSWebView/WEBVIEW/webview.aspx
Username: windtrial
Password: axyswind
The left hand window shows the station, which if you click on will expand out to show the messages (metocean and Waves) and if you click the + beside these you will get the individual data parameters which you can plot into a graph by selecting the checkbox of the parameter you want to graph and then clicking the Graph icon at the top of that window.
You can also see a table of the data by simply clicking on the message (click on the 1 MetOcean name and a table will appear on the RHS window with all the data) 

Times Colonist Article on Wind buoy deployed at RR

Sidney firm deploys world’s first wind buoy :
Times Colonist,October 28, 2009
http://www.timescolonist.com/technology/Sidney+firm+deploys+world+first+wind+buoy/2153639/story.html

Sidney’s AXYS Technologies has deployed the world’s first offshore wind resource assessment buoy near Race Rocks in order to test the machine prior to its commercial launch.

The WindSentinel was launched this week to compare wind data collected on the moving buoy to wind data collected from a station on Race Rocks about a half kilometre away.

The WindSentinel is designed to assist offshore wind farm developers in determining the available wind resource at potential wind farm sites. It is the world’s first wind resource assessment buoy capable of accurately measuring wind data at heights of conventional offshore wind turbines.

AXYS said wind farm developers have had to construct permanent offshore meteorological towers to do that work at an estimated cost of about $10 million. By contrast, a basic WindSentinel model is approximately $1 million.

The test site was chosen to thoroughly assess the buoy’s capabilities as the waters at Race Rocks see currents of between five and six knots, waves measuring between two and four metres high and winds up to 50 knots.

The results of the study are to be released in early 2010.

“The WindSentinel allows developers to collect crucial wind resource assessment data more accurately, more quickly and less expensively than every other available option,” said AXYS spokesman Dennis Stacey.
© Copyright (c) The Victoria Times Colonist

Test of AXYS Wind Assessment Technology

In October, 2009, Lester Pearson College had an opportunity to participate in an offshore wind assessment test by AXYS Technologies Inc. in the Strait of Juan de Fuca .

See video of test in Juan de Fuca off Race Rocks

Sidney firm deploys world’s first wind buoy :
Times Colonist,October 28, 2009

rm191009buoydeployed

The Wind Sentinnel deployed at Race Rocks on October 18, 2009 -Estimated duration is Oct. 16 – Nov. 16 (logistics/weather dependant) -Buoy Deployment Location – Lat: 48° 17.606’N Long: 123° 32.370’W -Communications – Buoy: Cellular phone -Communications – land station: Race Rocks LAN wired Ethernet connection

Great Race Rocks was used to host the land station for an offshore buoy which is designed to record  wind speed and direction data profiles up to 200 meters height. It is anchored outside of the Race Rocks Ecological Reserve in the Strait of Juan de Fuca. Data from the buoy is relayed automatically every 10 minutes by cell phone to the instrument trailer on land and is transmitted to the internet through our LAN on Race Rocks

 

 

https://www.racerocks.ca/wp-content/uploads/2009/09/AXYSWindSentinel.pdfLink to this brochure pdf with more specifications. AXYSWindSentinel

We will be able to benefit by adding the information collected to the knowledge base for the reserve. It will also be useful for planning for future sustainable energy applications.Our current wind measurements done by the Davis weather instrument we have installed on the ground level, often show at least a 10 km/h difference in wind velocity when compared with the Environment Canada data from the top of the tower at 36 metres. A set of data with projections to 200 metres will provide an excellent profile for comparisons.

See this sample file on Analyzing the data as an exercise.

Username: windtrial
Password: axyswind
The left hand window shows the station, which if you click on will expand out to show the messages (metocean and Waves) and if you click the + beside these you will get the individual data parameters which you can plot into a graph by selecting the checkbox of the parameter you want to graph and then clicking the Graph icon at the top of that window.

You can also see a table of the data by simply clicking on the message (click on the 1 MetOcean name and a table will appear on the RHS window with all the data)

Return to the Wind as an Abiotic Factor at Race Rocks File