Estimating early-winter Antarctic sea ice thickness from deformed ice morphology

被引:7
|
作者
Mei, M. Jeffrey [1 ,2 ]
Maksym, Ted [1 ]
Weissling, Blake [3 ]
Singh, Hanumant [4 ]
机构
[1] Woods Hole Oceanog Inst, Dept Appl Ocean Sci & Engn, Woods Hole, MA 02540 USA
[2] MIT, Dept Mech Engn, Cambridge, MA 02139 USA
[3] Univ Texas El Paso, Dept Geol Sci, El Paso, TX 79968 USA
[4] Northeastern Univ, Dept Elect & Comp Engn, Boston, MA 02115 USA
来源
CRYOSPHERE | 2019年 / 13卷 / 11期
基金
美国国家科学基金会;
关键词
AMUNDSEN SEAS; SNOW DEPTH; EAST ANTARCTICA; WEDDELL SEA; IN-SITU; BELLINGSHAUSEN; RETRIEVAL; FREEBOARD; ROUGHNESS; LAND;
D O I
10.5194/tc-13-2915-2019
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Satellites have documented variability in sea ice areal extent for decades, but there are significant challenges in obtaining analogous measurements for sea ice thickness data in the Antarctic, primarily due to difficulties in estimating snow cover on sea ice. Sea ice thickness (SIT) can be estimated from snow freeboard measurements, such as those from airborne/satellite lidar, by assuming some snow depth distribution or empirically fitting with limited data from drilled transects from various field studies. Current estimates for large-scale Antarctic SIT have errors as high as similar to 50 %, and simple statistical models of small-scale mean thickness have similarly high errors. Averaging measurements over hundreds of meters can improve the model fits to existing data, though these results do not necessarily generalize to other floes. At present, we do not have algorithms that accurately estimate SIT at high resolutions. We use a convolutional neural network with laser altimetry profiles of sea ice surfaces at 0.2m resolution to show that it is possible to estimate SIT at 20m resolution with better accuracy and generalization than current methods (mean relative errors similar to 15 %). Moreover, the neural network does not require specification of snow depth or density, which increases its potential applications to other lidar datasets. The learned features appear to correspond to basic morphological features, and these features appear to be common to other floes with the same climatology. This suggests that there is a relationship between the surface morphology and the ice thickness. The model has a mean relative error of 20% when applied to a new floe from the region and season. This method may be extended to lower-resolution, larger-footprint data such as such as Operation IceBridge, and it suggests a possible avenue to reduce errors in satellite estimates of Antarctic SIT from ICESat-2 over current methods, especially at smaller scales.
引用
收藏
页码:2915 / 2934
页数:20
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