Epoch |
Bathymetric Coverage |
Difference w.r.t previous
survey epoch |
Spring 2018 JD095 April 5, 6th |
overnighted at Steveston![]() reduced using observed Sand Heads tides. |
there are previous Heron surveys: 2017 2015 2013 2012 but I don't have the data with me right now. All difference maps have a greyscale that extends from -4m (black) to +4m (white) |
Fall 2018 JD291 October 17, 18th |
overnighted at Steveston![]() reduced using WebTide model |
difference - over summer 2018![]() +ve bias because the spring survey had a bad SV extension below 100m (MVP max depth) |
Spring 2019 JD110 April 20, 21st |
overnighted at Steveston![]() reduced using WebTide model |
difference - over winter
2018-2019![]() |
Fall 2019 JD279 October 6th |
transit home without Steveston
stop -weather too bad to do more than canyon ![]() reduced using WebTide model |
difference - over summer 2019![]() |
....... PANDEMIC DATA GAP ....... apparently there was:
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Winter 2021 JD340 December 14-15-16th |
about two weeks after the
once-a-century flood![]() reduced using Sand Heads predicted tides |
cumulative difference - two
summers - 2020 and 2021![]() I'd like to believe the distal Fraser Canyon activity (first since 2012) is due to the 100 year flood but could be anytime in summer 2020/1 |
Spring 2022 JD140 May 23, 24,25th |
river had just started to
rise..![]() reduced using Sand Heads predicted tides |
difference - over winter
2021-2022![]() striping is due to kmall PU bug not applying surface sound speed (needs reintegrating SVP) |
mid- summer 2022 JD17X June 26,27,28,29th |
river at full mid-summer
freshet (> 10,000 m3/s)![]() reduced using Sand Heads predicted tides ASCII lat--lon-depth file 2m grid spacing |
difference - first half of
summer 2022![]() surprisingly active distal Fraser canyon.. |