Revisiting Intertidal Transect sites at Race Rocks

Watden’s Report, September 3, 2021

I was fortunate to be able to get out to Race Rocks on one of the last morning low tides of the season. I wanted to revisit intertidal locations around the island in order to take photos of belt transects in locations I had recorded with baseline studies back in May of 1995. Photographic transects are valuable records in the event of changes that may happen along coastlines, usually caused by humans and/or by extreme weather events . 

 

Images taken in 1995 can be seen in this index on transects: https://racerocks.ca/ecology/ecological-monitoring/

The belt transect files with images will be linked here when they have been processed :

Peg 6  Peg5: Peg 5a  Peg 5b Peg 14a,  Peg 14b Peg 115. 

I was fortunate to have the assistance of Cedric Torres, the ecoguardian in doing the work on the transects.

 

At this time of year the island is populated by many young  glaucous-winged gulls, some fully fledged and other son various states of maturity. There were also a number of mortalities around the island which is typical for this time of year in a breeding colony.  In the following videos a number of behaviours of the chicks are shown .

Harbour seals with pups are hauled out on the southern most reef, note the current was still  ebbing in this video.

The California and Stellers sea lions have started coming back in large numbers. typically the Californias outnumber the Stelllers at this time of year.

Beneath the tower, the Californians( barking)  are predominant: but there is alos a mix of the growling Stellers.

 

On the East side cove a large group of Californian Sea lions were hauled out. The ones here were very skittish, any movement near the east end of the  house would startle them

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Other observations : two orcas in Race Passage ( surprizingly with no whale watching boats nearby.  The nice weather on Sept 3 brought out many whale watching boats and as usual they approach closer to the north side in front of the docks than necessary and well within the distance for viewing marine mammal colonies. The sea lions on that side are more habituated to the presence of humans and these boats than on other parts of the island, but many still go into an alert stage when the boats pass by.

Only a few pelagic cormorants were seen on the south west tip of the island.

The Calendula escapes from gardens of lightkeepers over 50 years ago still exist along the pathways, although the dry summer has been challenging. I was able to make a new species observation of these green blow flies on the flowers.

 

This summer with the heat dome experience on Vancouver Island there have been reports of damage to intertidal life. I took these images of high intertidal level barnacles in the arintertidal between peg 14 and 15. which show very little damage from this event,

We checked out Anita’s pool #6 . The intertidal life in the area has been unchanged for decades.

On the west side of the cliff near peg 5 , we took these images on the vertical rock face as records of barnacle distribution:

And near peg 15 we noted these finger limpets in a shaded rock at an extreme high intertidal elevation.

And a follow-up photo of The ill-fated tidepool #13 which was readjusted in the hurricane of 2006

 

 

 

 

 

Juan de Fuca CODAR System – Race Rocks (VROC) – Oceanographic Radar System

CODAR antenna at Race Rocks

Click on this image for the data display on the Ocean Networks Canada website:

CODAR SeaSonde continuous surface current mapping and wave monitoring HF radar system.

This is taken from this page: http://vocab.nerc.ac.uk/collection/L22/current/TOOL1366/

Seawater Salinity and Temperature, March, 2021

DAILY SEA SURFACE TEMPERATURE AND SALINITY OBSERVATIONS
Institute of Ocean Sciences, North Saanich, B.C., V8L 4B2
Station RACE ROCKS
Observer Rod King March
YSI ID: 24 Year: 2021
YSI YSI
Temp Sal
Day Time ºC ppt
1 15:00 7.9 32.1
2 19:00 7.9 31.9
3 9:00 7.5 31.6
4 17:30 7.8 31.4
5 20:10 7.8 31.7
6 20:37 7.7 31.6
7 19:59 7.7 31.6
8 21:08 7.7 31.5
9 23:30 7.8 31.5
10 13:00 8.0 31.0
11 11:38 8.0 31.5
12 10:40 8.0 31.5
13 10:00 8.0 31.5
14 18:00 8.0 31.6
15 19:21 8.0 31.6
16 21:27 8.0 31.9
17 20:22 7.8 32.0
18 21:10 7.9 31.9
19 20:23 7.9 31.5
20 19:12 7.9 31.4
21 8:20 7.9 31.5
22 9:07 7.8 31.4
23 11:37 7.8 31.4
24 11:01 8.0 31.0
25 11:11 8.0 31.2
26 20:12 8.1 31.4
27 16:00 8.2 31.6
28 15:50 8.2 31.4
29 22:50 8.0 31.5
30 18:11 8.2 31.8
31 20:05 8.2 31.7

Peregrine Falcon returns

Pam Birley from England took this image on the remote camera 5 today.  Almost yearly, she has spotted peregrines on Great Race Rocks using the remote control cameras . 

Falco peregrinus: Peregrine falcon –The Race Rocks Taxonomy

Seawater Data February, 2021

Daily Sea Surface Temperature and Salinity Observations
Station: Race Rocks
Observer: Rod King
Month: Feb-21
Day Time Temp °C Sal ppt
1 16:00 8.1 31.3
2 8:30 7.9 31.7
3 16:30 8.1 31.3
4 8:30 7.9 31.5
5 16:00 8.9 31.3
6 9:00 8.1 31.3
7 11:30 8 31.4
8 9:00 7.8 31.4
9 8:30 7.6 31.5
10 8:30 7.9 30.4
11 11:30 7.5 31.3
12 13:00 7.7 31.3
13 11:00 7.2 31.2
14 15:30 7.2 31.6
15 15:30 7.4 31.6
16 9:00 7.5 31.3
17 8:40 7.5 31.3
18 8:40 7.5 31.2
19 8:20 7.5 31.2
20 10:02 7.5 31.2
21 8:15 7.5 31.5
22 9:00 7.7 31.5
23 10:55 7.5 31.4
24 10:21 7.4 31.4
25 18:00 7.7 31.5
26 13:52 7.9 31.9
27 9:00 7.6 31.6
28 13:30 7.8 31.6
29
30
31

Why are the Waters around Race Rocks so Nutrient Rich?

The productivity of the waters passing by Race Rocks contributes to the high biodiversity and abundance of organisms in the area.  Part 5 of the following journal article provides a clue for the incidence of high Nitrogen level throughout the Strait of Juan de Fuca.

Free Access

Influences of the Juan de Fuca Eddy on circulation, nutrients, and phytoplankton production in the northern California Current System

First published: 06 August 2008

https://doi.org/10.1029/2007JC004412

Citations: 37

5. Regional Effects of the Juan de Fuca Eddy

5.1. Nutrient Enrichment of the Northern CCS

[44] The Juan de Fuca Eddy has been described as an “upwelling center”, allowing water to be raised from deeper depths than in classical wind‐driven upwelling [Freeland and Denman, 1982]. Upwelling in the eddy enriches the deep waters that flow into Juan de Fuca Strait as part of the estuarine circulation return flow. The penetration into the strait of this nutrient‐rich water mass is evident in a vertical section of ambient nitrate concentration measured in September 2003 (Figure 13). At the mouth of the strait, nitrate concentrations below 100 m (the approximate depth of the division between inflow and outflow) are >34 μM. Similar concentrations are present in bottom water along the strait axis, reaching ∼150 km east of the Strait entrance where strong mixing in shallow regions of high tidal currents mixes them upwards.

image

Vertical section of nitrate concentration measured in an along‐axis Juan de Fuca Strait transect (18 September 2003). Station names are across the top of the section and geographically in the insert figure. Continue reading

Pigeon Guillemots Return to Nesting Grounds.

Pam Birley of England made the first observation today for this year using the remote control camera 5, of the return of the pigeon guillemots to their nesting  grounds here on Race Rocks . She commented: “I haven’t seen them mentioned by the guardian yet but I took this screenshot on 3rd Feb”.