Comments (1)
Attaching my slides from the OMO meeting here. Morrison_ASC_heat_transport.pdf
For the Getz and Totten transects, it looks like the velocity structure in the Totten remains unchanged between strong and weak ASC, while the ASC penetrates deeper in the Getz while it speeds up. Velocities on the Totten are also much greater than on Getz.
Could there be a threshold where for a weaker ASC, the CSHT and ASC speed are correlated, while for stronger ASC there is little difference? i.e. for ASC stronger than a certain threshold, the along-isopycnal pathway for CDW intrusions is still blocked, at least on an interannual timescale? I guess this is kind of inline with what you were thinking @adele-morrison, where the changing sign of the ASC could make a difference.
Based on Adele's results, I redid the correlations only including locations where the ASC speed remains below a certain threshold in the given time series (mask has dimensions (lon_bins, density)). The hypothesis is that regions with lower ASC speed have greater correlations.
Since we mainly care about the CDW layer, the filled plot shows the correlations in the CDW layer for locations where the ASC speed is below a threshold velocity. As the threshold increases, more longitudinal bins are included. Although the highest correlation regions are included at lower thresholds, the link between low threshold speed and high correlation does not hold past threshold u= 0.05m/s. Even when looking at threshold u = 0.04 m/s, there are still regions of lower correlation (r^2 ~ 0.3-0.45) that are included. The threshold velocity I think could be an explanation for the lack of correlation in certain regions e.g. Totten, but definitely is not the full story.
The blank spaces are explained by the lower panel, with the correlations in each density layer. In the blank regions, the CDW layer does not exist, which might be filled by the correlation of the next densest layer. So in the WAP and Weddell, the water at the 1000m isobath is lighter than the 27.82 kg/m3 bin.
The same plot as above using annual averaged correlations is below:
Motivating slide from Adele's presentation below:
from asc_and_heat_transport.
Related Issues (20)
- Fix zonal convergence of heat transport around peninsula [ Task 5] HOT 3
- Cross-slope heat transport calculation method HOT 6
- Cross-slope heat transport using different methods to extract an isobath HOT 6
- Poster for IUGG
- Identifying ASC Regimes and variability HOT 45
- Zonal convergence bias in vertical profiles of CSHT HOT 6
- Analysis of individual sub-regimes HOT 6
- Alternative plots visualizations HOT 6
- Figure discussion for paper HOT 4
- Recreate figures with time-mean regime masks HOT 3
- Statistics using longitude bins before averaging over distinct ASC regimes HOT 29
- Depth normalisation HOT 21
- Reduce bin size when longitude-binning CSHT and U_along HOT 4
- Presenting these results at conferences HOT 11
- Missing data at longitude edges HOT 10
- Choice of vertical coordinate / depth range of importance HOT 6
- New visualisation of cross-slope properties in Antarctic margins? HOT 7
- Bining of ASC speed into sigma increase maximums HOT 4
- Defining sigma levels according to water mass properties HOT 18
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from asc_and_heat_transport.