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S.R.M.L. and M.R.v.d.B. contributed the calculations of firn layer depths.
Complementary site data including the results of drilling and active layer depths measurements were also obtained.
The corresponding active layer depths varied from 2.45 to 1.80 m.
A similar relationship was formed between pstS expression and the previous-day aerosol particles, but nonexistent regarding mixed layer depths.
The most active water and heat exchange occurs in the upper soil layer (depths of 0 25 cm).
The changes are overall relatively weak, except for mixed layer depths, which are in general excessively reduced compared to observation-based estimates.
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Average active layer depth along this transect is 0.37 m.
The effects of firn layer depth variability on elevation are calculated by a firn densification model33.
Acoustic sounders are used primarily to monitor boundary layer depth and structure, using echo-return characteristics.
The available variables include salinity, temperature, potential temperature, and mixed layer depth.
IGOSS sio climatology: Climatological heat storage, mixed layer depth, and temperature data from Scripps Institution of Oceanography.
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