Open mmr0 opened 10 months ago
Box 1 lats = array([-65.4987, -65.7091, -65.6935, -65.4519]) lons = array([97.8152, 97.8152, 98.2762, 98.2574])
Box 2 lats = array([-65.3273, -65.5688, -65.561 , -65.2961]) lons = array([98.5867, 98.6337, 99.1606, 99.123 ])
Map:
T-S over 2000-2018 (monthly data):
Only Januarys:
Looks like some CDW coming in in Box2 but not in Box1?
MITgcm, RYF (1990-91), BedMachine bathymetry Map: (be careful the depth is the ocean depth or the ocean thickness - there is an ice shelf on the top of the ocean layer in the ice shelf region.) TS diagrams: Looks water masses in MITgcm are much colder than ACCESS :)
Yiew, thanks @claireyung @yuhang559, this is awesome! Yeah it looks like Boxes 1 and 2 are pretty similar except for Box 1 being much shallower and excluding CDW in ACCESS and mostly excluding it in MITgcm. We definitely didn't catch any ISW haha. How do I interpret all this near-freezing point fresher water in MITgcm e.g. in Box 2 in Jan? is this freshwater from melted sea ice?
Some papers:
Ribiero et al 2023 - Change in watermass properties east of Shackleton from historical -> recent data https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JC019882
Van Wijk 2022 - CDW observed in trough in front of/adjacent to Denman Ice Tongue from profiling floats https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2022GL100460
Yiew, thanks @claireyung @yuhang559, this is awesome! Yeah it looks like Boxes 1 and 2 are pretty similar except for Box 1 being much shallower and excluding CDW in ACCESS and mostly excluding it in MITgcm. We definitely didn't catch any ISW haha. How do I interpret all this near-freezing point fresher water in MITgcm e.g. in Box 2 in Jan? is this freshwater from melted sea ice?
Yes, the freshwater in MITgcm is both from the sea ice and the melting of the ice shelf.
MITgcm(RYF, tides) Current speed and two summer sections
Velocity map:
Velocity-depth figure (white circle in velocity map): Our model includes the tides, but we only save the monthly mean data, so it probably can't capture the tide variability and the velocity-depth figure shows the velocity is highly sensitive to the position of the dots.
TS diagram sections: To plot it conveniently, I interpolated the matrix, so section 1 and section 2 look in different resolutions.
Thanks so much Yuhang, this is super useful!
MITgcm(RYF, tides) Current speed and two summer sections
Velocity map:
Velocity-depth figure (white circle in velocity map): Our model includes the tides, but we only save the monthly mean data, so it probably can't capture the tide variability and the velocity-depth figure shows the velocity is highly sensitive to the position of the dots.
TS diagram sections: To plot it conveniently, I interpolated the matrix, so section 1 and section 2 look in different resolutions.
What do we expect to see at our Shackleton sampling/mooring site?
Wish list for pre-departure
Ideas for later
When? Campaign is early Jan, so summer data is most relevant. Would be interested to see summer vs winter perhaps?
Brief summary of the Hot Water Drilling: One borehole through the Shackleton Ice Shelf, near the western flank of the Denman Ice Shelf. Ice approx 200m thick, water column total depth ~600m, TBC. Data sampling will include CTD profiling, water sample collection, video logging and sediment collection. Following profiling, we will deploy a mooring with 2 x CTD (one near ice-ocean interface and one near seafloor, sampling @ 10 minute intervals) and 1 x current meter (near ice-ocean interface, sampling @ 30 minute intervals), and a distributed temperature sensing (DTS) fibre optic cable which will give meter-resolution temperature through both the ice and water column. Expected endurance of the ocean instruments is ~ 3 years. DTS data will be 1 year. At the surface, an APRES will collect basal melt rate data.
What do we expect to see near Duanne's epishelf lake sites?
Wish list:
Any help on any of these would be amazing!!