A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea

The snow depth on Antarctic sea ice is critical to estimating the sea ice thickness distribution from laser altimetry data, such as from Operation IceBridge or ICESat-2. Snow redistributed by wind collects around areas of deformed ice and forms a wide variety of feature on sea ice; the morphology of...

Full description

Bibliographic Details
Main Authors: M. Jeffrey Mei, Ted Maksym
Format: Article
Language:English
Published: MDPI AG 2020-05-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/9/1494
id doaj-0df9e7b01ecd4b4792cb8488cea8359b
record_format Article
spelling doaj-0df9e7b01ecd4b4792cb8488cea8359b2020-11-25T02:12:10ZengMDPI AGRemote Sensing2072-42922020-05-01121494149410.3390/rs12091494A Textural Approach to Improving Snow Depth Estimates in the Weddell SeaM. Jeffrey Mei0Ted Maksym1Department of Applied Ocean Science and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02540, USADepartment of Applied Ocean Science and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02540, USAThe snow depth on Antarctic sea ice is critical to estimating the sea ice thickness distribution from laser altimetry data, such as from Operation IceBridge or ICESat-2. Snow redistributed by wind collects around areas of deformed ice and forms a wide variety of feature on sea ice; the morphology of these features may provide some indication of the mean snow depth. Here, we apply a textural segmentation algorithm to classify and group similar textures to infer the distribution of snow using snow surface freeboard measurements from Operation IceBridge campaigns over the Weddell Sea. We find that texturally-similar regions have similar snow/ice ratios, even when they have different absolute snow depth measurements. This allows for the extrapolation of nadir-looking snow radar data using two-dimensional surface altimetry scans, providing a two-dimensional estimate of the snow depth with ∼22% error. We show that at the floe scale (∼180 m), snow depth can be directly estimated from the snow surface with ∼20% error using deep learning techniques, and that the learned filters are comparable to standard textural analysis techniques. This error drops to ∼14% when averaged over 1.5 km scales. These results suggest that surface morphological information can improve remotely-sensed estimates of snow depth, and hence sea ice thickness, as compared to current methods. Such methods may be useful for reducing uncertainty in Antarctic sea ice thickness estimates from ICESat-2.https://www.mdpi.com/2072-4292/12/9/1494sea icemorphologytexturesegmentationsnow depth
collection DOAJ
language English
format Article
sources DOAJ
author M. Jeffrey Mei
Ted Maksym
spellingShingle M. Jeffrey Mei
Ted Maksym
A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea
Remote Sensing
sea ice
morphology
texture
segmentation
snow depth
author_facet M. Jeffrey Mei
Ted Maksym
author_sort M. Jeffrey Mei
title A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea
title_short A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea
title_full A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea
title_fullStr A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea
title_full_unstemmed A Textural Approach to Improving Snow Depth Estimates in the Weddell Sea
title_sort textural approach to improving snow depth estimates in the weddell sea
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-05-01
description The snow depth on Antarctic sea ice is critical to estimating the sea ice thickness distribution from laser altimetry data, such as from Operation IceBridge or ICESat-2. Snow redistributed by wind collects around areas of deformed ice and forms a wide variety of feature on sea ice; the morphology of these features may provide some indication of the mean snow depth. Here, we apply a textural segmentation algorithm to classify and group similar textures to infer the distribution of snow using snow surface freeboard measurements from Operation IceBridge campaigns over the Weddell Sea. We find that texturally-similar regions have similar snow/ice ratios, even when they have different absolute snow depth measurements. This allows for the extrapolation of nadir-looking snow radar data using two-dimensional surface altimetry scans, providing a two-dimensional estimate of the snow depth with ∼22% error. We show that at the floe scale (∼180 m), snow depth can be directly estimated from the snow surface with ∼20% error using deep learning techniques, and that the learned filters are comparable to standard textural analysis techniques. This error drops to ∼14% when averaged over 1.5 km scales. These results suggest that surface morphological information can improve remotely-sensed estimates of snow depth, and hence sea ice thickness, as compared to current methods. Such methods may be useful for reducing uncertainty in Antarctic sea ice thickness estimates from ICESat-2.
topic sea ice
morphology
texture
segmentation
snow depth
url https://www.mdpi.com/2072-4292/12/9/1494
work_keys_str_mv AT mjeffreymei atexturalapproachtoimprovingsnowdepthestimatesintheweddellsea
AT tedmaksym atexturalapproachtoimprovingsnowdepthestimatesintheweddellsea
AT mjeffreymei texturalapproachtoimprovingsnowdepthestimatesintheweddellsea
AT tedmaksym texturalapproachtoimprovingsnowdepthestimatesintheweddellsea
_version_ 1724911131010531328