Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China

Snow cover plays an important role in hydrological processes and seasonal water balance. Especially in the Tibetan Plateau (TP), snow cover is an important source of the Yangtze River, Yellow River and Lancang River (SRYYL), which greatly influences regional water balance. In this study, we quantifi...

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Main Authors: Siyuan Wang, Hang Yin, Qichun Yang, Hui Yin, Xiaoyue Wang, Yaoyao Peng, Ming Shen
Format: Article
Language:English
Published: Taylor & Francis Group 2017-05-01
Series:International Journal of Digital Earth
Subjects:
Online Access:http://dx.doi.org/10.1080/17538947.2016.1231229
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author Siyuan Wang
Hang Yin
Qichun Yang
Hui Yin
Xiaoyue Wang
Yaoyao Peng
Ming Shen
author_facet Siyuan Wang
Hang Yin
Qichun Yang
Hui Yin
Xiaoyue Wang
Yaoyao Peng
Ming Shen
author_sort Siyuan Wang
collection DOAJ
description Snow cover plays an important role in hydrological processes and seasonal water balance. Especially in the Tibetan Plateau (TP), snow cover is an important source of the Yangtze River, Yellow River and Lancang River (SRYYL), which greatly influences regional water balance. In this study, we quantified the temporal trend and spatial variation of snow cover across the TP by calibrating and developing the Advance Very High Resolution Radiometer (AVHRR) Long Term Data Record (LTDR)-derived snow cover products during 1982-2011. We also examined the relationship of snow cover with temperature and precipitation over the TP during 1982–2011. The results indicate that seasonal snow cover generally starts to accumulate from central plateau in October, while significant melting starts to occur from the southeastern plateau in May of following year. The long-term variability of snow cover is characterized by the tendency for a slight decrease in the mean snow coverage during the period of hydrological year (HY) 1982–1993 and a slight increase from HY2001 to 2011, but the total snow cover area remains relatively stable over the past 30 years. The results also show that temperature plays a critical role in controlling the snow cover days.
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spelling doaj.art-b7e40d5a5496411193ba6d78b80602342023-09-21T14:38:05ZengTaylor & Francis GroupInternational Journal of Digital Earth1753-89471753-89552017-05-0110550452110.1080/17538947.2016.12312291231229Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, ChinaSiyuan Wang0Hang Yin1Qichun Yang2Hui Yin3Xiaoyue Wang4Yaoyao Peng5Ming Shen6Institute of Remote Sensing and Digital Earth, Chinese Academy of ScienceInstitute of Remote Sensing and Digital Earth, Chinese Academy of SciencePacific Northwest National LaboratoryInstitute of Remote Sensing and Digital Earth, Chinese Academy of ScienceInstitute of Remote Sensing and Digital Earth, Chinese Academy of ScienceInstitute of Remote Sensing and Digital Earth, Chinese Academy of ScienceInstitute of Remote Sensing and Digital Earth, Chinese Academy of ScienceSnow cover plays an important role in hydrological processes and seasonal water balance. Especially in the Tibetan Plateau (TP), snow cover is an important source of the Yangtze River, Yellow River and Lancang River (SRYYL), which greatly influences regional water balance. In this study, we quantified the temporal trend and spatial variation of snow cover across the TP by calibrating and developing the Advance Very High Resolution Radiometer (AVHRR) Long Term Data Record (LTDR)-derived snow cover products during 1982-2011. We also examined the relationship of snow cover with temperature and precipitation over the TP during 1982–2011. The results indicate that seasonal snow cover generally starts to accumulate from central plateau in October, while significant melting starts to occur from the southeastern plateau in May of following year. The long-term variability of snow cover is characterized by the tendency for a slight decrease in the mean snow coverage during the period of hydrological year (HY) 1982–1993 and a slight increase from HY2001 to 2011, but the total snow cover area remains relatively stable over the past 30 years. The results also show that temperature plays a critical role in controlling the snow cover days.http://dx.doi.org/10.1080/17538947.2016.1231229snow covertemporal-spatial variationnoaa-avhrr ltdrtibetan plateau
spellingShingle Siyuan Wang
Hang Yin
Qichun Yang
Hui Yin
Xiaoyue Wang
Yaoyao Peng
Ming Shen
Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China
International Journal of Digital Earth
snow cover
temporal-spatial variation
noaa-avhrr ltdr
tibetan plateau
title Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China
title_full Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China
title_fullStr Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China
title_full_unstemmed Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China
title_short Spatiotemporal patterns of snow cover retrieved from NOAA-AVHRR LTDR: a case study in the Tibetan Plateau, China
title_sort spatiotemporal patterns of snow cover retrieved from noaa avhrr ltdr a case study in the tibetan plateau china
topic snow cover
temporal-spatial variation
noaa-avhrr ltdr
tibetan plateau
url http://dx.doi.org/10.1080/17538947.2016.1231229
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