Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019
A long-term dataset of 38 years (1982–2019) from the Advanced Very High Resolution Radiometer (AVHRR) satellite observations is applied to investigate the spatio-temporal seasonal trends in cloud fraction, surface downwelling longwave flux, and surface upwelling longwave flux over the Arctic seas (6...
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doaj-fb19dd6e57f2460bbdb7fdf5356f8cbb2021-08-26T14:17:37ZengMDPI AGRemote Sensing2072-42922021-08-01133201320110.3390/rs13163201Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019Xi Wang0Jian Liu1Bingyun Yang2Yansong Bao3George P. Petropoulos4Hui Liu5Bo Hu6National Satellite Meteorological Center, Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, China Meteorological Administration, Beijing 100081, ChinaNational Satellite Meteorological Center, Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, China Meteorological Administration, Beijing 100081, ChinaNational Satellite Meteorological Center, Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, China Meteorological Administration, Beijing 100081, ChinaCollaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, CMA Key Laboratory for Aerosol-Cloud-Precipitation, Nanjing University of Information Science & Technology, Nanjing 210044, ChinaDepartment of Geography, Harokopio University of Athens, EI. Venizelou 70, Kallithea, 17671 Athens, GreeceNational Satellite Meteorological Center, Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, China Meteorological Administration, Beijing 100081, ChinaNingbo Meteorological Administration, Ningbo 315012, ChinaA long-term dataset of 38 years (1982–2019) from the Advanced Very High Resolution Radiometer (AVHRR) satellite observations is applied to investigate the spatio-temporal seasonal trends in cloud fraction, surface downwelling longwave flux, and surface upwelling longwave flux over the Arctic seas (60~90° N) by the non-parametric methods. The results presented here provide a further contribution to understand the cloud cover and longwave surface radiation trends over the Arctic seas, and their correlations to the shrinking sea ice. Our results suggest that the cloud fraction shows a positive trend for all seasons since 2008. Both surface downwelling and upwelling longwave fluxes present significant positive trends since 1982 with higher magnitudes in autumn and winter. The spatial distribution of the trends is nearly consistent between the cloud fraction and the surface longwave radiation, except for spring over the Chukchi and Beaufort Seas. We further obtained a significant negative correlation between cloud fraction (surface downwelling/upwelling longwave fluxes) and sea-ice concentration during autumn, which is largest in magnitude for regions with substantial sea ice retreat. We found that the negative correlation between cloud fraction and sea-ice concentration is not as strong as that for the surface downwelling longwave flux. It indicates the increase in cloudiness may result in positive anomalies in surface downwelling longwave flux which is highly correlated with the sea-ice retreat in autumn.https://www.mdpi.com/2072-4292/13/16/3201Arcticcloud fractionsurface longwave fluxseasonal trendAPP-x |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Xi Wang Jian Liu Bingyun Yang Yansong Bao George P. Petropoulos Hui Liu Bo Hu |
spellingShingle |
Xi Wang Jian Liu Bingyun Yang Yansong Bao George P. Petropoulos Hui Liu Bo Hu Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019 Remote Sensing Arctic cloud fraction surface longwave flux seasonal trend APP-x |
author_facet |
Xi Wang Jian Liu Bingyun Yang Yansong Bao George P. Petropoulos Hui Liu Bo Hu |
author_sort |
Xi Wang |
title |
Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019 |
title_short |
Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019 |
title_full |
Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019 |
title_fullStr |
Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019 |
title_full_unstemmed |
Seasonal Trends in Clouds and Radiation over the Arctic Seas from Satellite Observations during 1982 to 2019 |
title_sort |
seasonal trends in clouds and radiation over the arctic seas from satellite observations during 1982 to 2019 |
publisher |
MDPI AG |
series |
Remote Sensing |
issn |
2072-4292 |
publishDate |
2021-08-01 |
description |
A long-term dataset of 38 years (1982–2019) from the Advanced Very High Resolution Radiometer (AVHRR) satellite observations is applied to investigate the spatio-temporal seasonal trends in cloud fraction, surface downwelling longwave flux, and surface upwelling longwave flux over the Arctic seas (60~90° N) by the non-parametric methods. The results presented here provide a further contribution to understand the cloud cover and longwave surface radiation trends over the Arctic seas, and their correlations to the shrinking sea ice. Our results suggest that the cloud fraction shows a positive trend for all seasons since 2008. Both surface downwelling and upwelling longwave fluxes present significant positive trends since 1982 with higher magnitudes in autumn and winter. The spatial distribution of the trends is nearly consistent between the cloud fraction and the surface longwave radiation, except for spring over the Chukchi and Beaufort Seas. We further obtained a significant negative correlation between cloud fraction (surface downwelling/upwelling longwave fluxes) and sea-ice concentration during autumn, which is largest in magnitude for regions with substantial sea ice retreat. We found that the negative correlation between cloud fraction and sea-ice concentration is not as strong as that for the surface downwelling longwave flux. It indicates the increase in cloudiness may result in positive anomalies in surface downwelling longwave flux which is highly correlated with the sea-ice retreat in autumn. |
topic |
Arctic cloud fraction surface longwave flux seasonal trend APP-x |
url |
https://www.mdpi.com/2072-4292/13/16/3201 |
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