Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau

In the Tibetan Plateau (TP), the changes of lake ice phenology not only reflect regional climate change, but also impose substantial ecohydrological impacts on the local environment. Due to the limitation of ground observation, remote sensing has been used as an alternative tool to investigate recen...

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Main Authors: Linan Guo, Yanhong Wu, Hongxing Zheng, Bing Zhang, Junsheng Li, Fangfang Zhang, Qian Shen
Format: Article
Language:English
Published: MDPI AG 2018-09-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/10/10/1534
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author Linan Guo
Yanhong Wu
Hongxing Zheng
Bing Zhang
Junsheng Li
Fangfang Zhang
Qian Shen
author_facet Linan Guo
Yanhong Wu
Hongxing Zheng
Bing Zhang
Junsheng Li
Fangfang Zhang
Qian Shen
author_sort Linan Guo
collection DOAJ
description In the Tibetan Plateau (TP), the changes of lake ice phenology not only reflect regional climate change, but also impose substantial ecohydrological impacts on the local environment. Due to the limitation of ground observation, remote sensing has been used as an alternative tool to investigate recent changes of lake ice phenology. However, uncertainties exist in the remotely sensed lake ice phenology owing to both the data and methods used. In this paper, three different remotely sensed datasets are used to investigate the lake ice phenology variation in the past decade across the Tibetan Plateau, with the consideration of the underlying uncertainties. The remotely sensed data used include reflectance data, snow product, and land surface temperature (LST) data of moderate resolution imaging spectroradiometer (MODIS). The uncertainties of the three methods based on the corresponding data are assessed using the triple collocation approach. Comparatively, it is found that the method based on reflectance data outperforms the other two methods. The three methods are more consistent in determining the thawing dates rather than the freezing dates of lake ice. It is consistently shown by the three methods that the ice-covering duration in the northern part of the TP lasts longer than that in the south. Though there is no general trend of lake ice phenology across the TP for the period of 2000–2015, the warmer climate and stronger wind have led to the earlier break-up of lake ice.
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spelling doaj.art-4d12e3f7092841f380a386738bad14c32022-12-21T17:18:13ZengMDPI AGRemote Sensing2072-42922018-09-011010153410.3390/rs10101534rs10101534Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan PlateauLinan Guo0Yanhong Wu1Hongxing Zheng2Bing Zhang3Junsheng Li4Fangfang Zhang5Qian Shen6Key Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Science, Beijing 100094, ChinaKey Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Science, Beijing 100094, ChinaCSIRO Land and Water, Canberra, ACT 2601, AustraliaKey Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Science, Beijing 100094, ChinaKey Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Science, Beijing 100094, ChinaKey Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Science, Beijing 100094, ChinaKey Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Science, Beijing 100094, ChinaIn the Tibetan Plateau (TP), the changes of lake ice phenology not only reflect regional climate change, but also impose substantial ecohydrological impacts on the local environment. Due to the limitation of ground observation, remote sensing has been used as an alternative tool to investigate recent changes of lake ice phenology. However, uncertainties exist in the remotely sensed lake ice phenology owing to both the data and methods used. In this paper, three different remotely sensed datasets are used to investigate the lake ice phenology variation in the past decade across the Tibetan Plateau, with the consideration of the underlying uncertainties. The remotely sensed data used include reflectance data, snow product, and land surface temperature (LST) data of moderate resolution imaging spectroradiometer (MODIS). The uncertainties of the three methods based on the corresponding data are assessed using the triple collocation approach. Comparatively, it is found that the method based on reflectance data outperforms the other two methods. The three methods are more consistent in determining the thawing dates rather than the freezing dates of lake ice. It is consistently shown by the three methods that the ice-covering duration in the northern part of the TP lasts longer than that in the south. Though there is no general trend of lake ice phenology across the TP for the period of 2000–2015, the warmer climate and stronger wind have led to the earlier break-up of lake ice.http://www.mdpi.com/2072-4292/10/10/1534lake ice phenologyTibetan Plateauinland waterclimate change
spellingShingle Linan Guo
Yanhong Wu
Hongxing Zheng
Bing Zhang
Junsheng Li
Fangfang Zhang
Qian Shen
Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau
Remote Sensing
lake ice phenology
Tibetan Plateau
inland water
climate change
title Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau
title_full Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau
title_fullStr Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau
title_full_unstemmed Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau
title_short Uncertainty and Variation of Remotely Sensed Lake Ice Phenology across the Tibetan Plateau
title_sort uncertainty and variation of remotely sensed lake ice phenology across the tibetan plateau
topic lake ice phenology
Tibetan Plateau
inland water
climate change
url http://www.mdpi.com/2072-4292/10/10/1534
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