Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites

The opacity of clouds is the main problem for optical and thermal space-borne sensors, like the Moderate-Resolution Imaging Spectroradiometer (MODIS). Especially during polar nighttime, the low thermal contrast between clouds and the underlying snow/ice results in deficiencies of the MODIS cloud mas...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Stephan Paul, Sascha Willmes, Oliver Gutjahr, Andreas Preußer, Günther Heinemann
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2015
Subjects:
Online Access:https://doi.org/10.3390/rs70505042
id ftmdpi:oai:mdpi.com:/2072-4292/7/5/5042/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/7/5/5042/ 2023-08-20T04:02:31+02:00 Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites Stephan Paul Sascha Willmes Oliver Gutjahr Andreas Preußer Günther Heinemann agris 2015-04-23 application/pdf https://doi.org/10.3390/rs70505042 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs70505042 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 7; Issue 5; Pages: 5042-5056 MODIS polynyas sea ice clouds gap filling Text 2015 ftmdpi https://doi.org/10.3390/rs70505042 2023-07-31T20:43:11Z The opacity of clouds is the main problem for optical and thermal space-borne sensors, like the Moderate-Resolution Imaging Spectroradiometer (MODIS). Especially during polar nighttime, the low thermal contrast between clouds and the underlying snow/ice results in deficiencies of the MODIS cloud mask and affected products. There are different approaches to retrieve information about frequently cloud-covered areas, which often operate with large amounts of days aggregated into single composites for a long period of time. These approaches are well suited for static-nature, slow changing surface features (e.g., fast-ice extent). However, this is not applicable to fast-changing features, like sea-ice polynyas. Therefore, we developed a spatial feature reconstruction to derive information for cloud-covered sea-ice areas based on the surrounding days weighted directly proportional with their temporal proximity to the initial day of interest. Its performance is tested based on manually-screened and artificially cloud-covered case studies of MODIS-derived polynya area data for the polynya in the Brunt Ice Shelf region of Antarctica. On average, we are able to completely restore the artificially cloud-covered test areas with a spatial correlation of 0.83 and a mean absolute spatial deviation of 21%. Text Antarc* Antarctica Brunt Ice Shelf Ice Shelf Sea ice MDPI Open Access Publishing Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) Remote Sensing 7 5 5042 5056
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic MODIS
polynyas
sea ice
clouds
gap filling
spellingShingle MODIS
polynyas
sea ice
clouds
gap filling
Stephan Paul
Sascha Willmes
Oliver Gutjahr
Andreas Preußer
Günther Heinemann
Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites
topic_facet MODIS
polynyas
sea ice
clouds
gap filling
description The opacity of clouds is the main problem for optical and thermal space-borne sensors, like the Moderate-Resolution Imaging Spectroradiometer (MODIS). Especially during polar nighttime, the low thermal contrast between clouds and the underlying snow/ice results in deficiencies of the MODIS cloud mask and affected products. There are different approaches to retrieve information about frequently cloud-covered areas, which often operate with large amounts of days aggregated into single composites for a long period of time. These approaches are well suited for static-nature, slow changing surface features (e.g., fast-ice extent). However, this is not applicable to fast-changing features, like sea-ice polynyas. Therefore, we developed a spatial feature reconstruction to derive information for cloud-covered sea-ice areas based on the surrounding days weighted directly proportional with their temporal proximity to the initial day of interest. Its performance is tested based on manually-screened and artificially cloud-covered case studies of MODIS-derived polynya area data for the polynya in the Brunt Ice Shelf region of Antarctica. On average, we are able to completely restore the artificially cloud-covered test areas with a spatial correlation of 0.83 and a mean absolute spatial deviation of 21%.
format Text
author Stephan Paul
Sascha Willmes
Oliver Gutjahr
Andreas Preußer
Günther Heinemann
author_facet Stephan Paul
Sascha Willmes
Oliver Gutjahr
Andreas Preußer
Günther Heinemann
author_sort Stephan Paul
title Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites
title_short Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites
title_full Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites
title_fullStr Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites
title_full_unstemmed Spatial Feature Reconstruction of Cloud-Covered Areas in Daily MODIS Composites
title_sort spatial feature reconstruction of cloud-covered areas in daily modis composites
publisher Multidisciplinary Digital Publishing Institute
publishDate 2015
url https://doi.org/10.3390/rs70505042
op_coverage agris
long_lat ENVELOPE(-22.500,-22.500,-74.750,-74.750)
geographic Brunt Ice Shelf
geographic_facet Brunt Ice Shelf
genre Antarc*
Antarctica
Brunt Ice Shelf
Ice Shelf
Sea ice
genre_facet Antarc*
Antarctica
Brunt Ice Shelf
Ice Shelf
Sea ice
op_source Remote Sensing; Volume 7; Issue 5; Pages: 5042-5056
op_relation https://dx.doi.org/10.3390/rs70505042
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs70505042
container_title Remote Sensing
container_volume 7
container_issue 5
container_start_page 5042
op_container_end_page 5056
_version_ 1774713015786012672