Abstract. Snow over sea ice controls energy budgets and affects sea
ice growth and melting and thus has essential effects on the climate. Passive
microwave radiometers can be used for basin-scale snow depth estimation at a
daily scale; however, previously published methods applied to the Antarctic
clearly underestimated snow depth, limiting their further application. Here,
we estimated snow depth using passive microwave radiometers and a newly
constructed, robust method by incorporating lower frequencies, which have
been available from AMSR-E and AMSR-2 since 2002. A regression analysis
using 7 years of Operation IceBridge (OIB) airborne snow depth measurements
showed that the gradient ratio (GR) calculated using brightness temperatures
in vertically polarized 37 and 7 GHz, i.e. GR(37/7), was optimal for
deriving Antarctic snow depth, with a correlation coefficient of −0.64. We
hence derived new coefficients based on GR(37/7) to improve the current snow
depth estimation from passive microwave radiometers. Comparing the new
retrieval with in situ measurements from the Australian Antarctic Data
Centre showed that this method outperformed the previously available method
(i.e. linear regression model based on GR(37/19)), with a mean difference
of 5.64 cm and an RMSD of 13.79 cm, compared to values of −14.47 and
19.49 cm, respectively. A comparison to shipborne observations from
Antarctic Sea Ice Processes and Climate indicated that in thin-ice regions,
the proposed method performed slightly better than the previous method (with
RMSDs of 16.85 and 17.61 cm, respectively). We generated a complete snow
depth product over Antarctic sea ice from 2002 to 2020 on a daily scale, and
negative trends could be found in all sea sectors and seasons. This dataset
(including both snow depth and snow depth uncertainty) can be downloaded
from the National Tibetan Plateau Data Center, Institute of Tibetan Plateau
Research, Chinese Academy of Sciences at
http://data.tpdc.ac.cn/en/disallow/61ea8177-7177-4507-aeeb-0c7b653d6fc3/ (last access: 7 February 2022)
(Shen and Ke, 2021, https://doi.org/10.11888/Snow.tpdc.271653).