Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau

Abstract Lake ice is a sensitive factor for the Earth’s environment and climate change research. In the comparative study on climate change to the Earth three-pole (Antarctic, Arctic, and Tibetan Plateau), the lake ice phenology can be used to represent seasonal climate changes. In this paper, the l...

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Published in:IOP Conference Series: Earth and Environmental Science
Main Authors: Xingxing, Wang, Yubao, Qiu, Lemmetyinen, Juha, Pengfei, Xie, Cheng, Bin, Wenshan, Liang
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2020
Subjects:
Online Access:http://dx.doi.org/10.1088/1755-1315/502/1/012033
https://iopscience.iop.org/article/10.1088/1755-1315/502/1/012033/pdf
https://iopscience.iop.org/article/10.1088/1755-1315/502/1/012033
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spelling crioppubl:10.1088/1755-1315/502/1/012033 2024-09-15T17:41:46+00:00 Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau Xingxing, Wang Yubao, Qiu Lemmetyinen, Juha Pengfei, Xie Cheng, Bin Wenshan, Liang 2020 http://dx.doi.org/10.1088/1755-1315/502/1/012033 https://iopscience.iop.org/article/10.1088/1755-1315/502/1/012033/pdf https://iopscience.iop.org/article/10.1088/1755-1315/502/1/012033 unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 502, issue 1, page 012033 ISSN 1755-1307 1755-1315 journal-article 2020 crioppubl https://doi.org/10.1088/1755-1315/502/1/012033 2024-07-22T04:16:35Z Abstract Lake ice is a sensitive factor for the Earth’s environment and climate change research. In the comparative study on climate change to the Earth three-pole (Antarctic, Arctic, and Tibetan Plateau), the lake ice phenology can be used to represent seasonal climate changes. In this paper, the lake ice phenology and the corresponding daily temperature for 48 lakes in Northern Europe, Tibetan Plateau and Mongolia Plateau were used as the typical case for comparative research. Based on passive microwave remote sensing data. The results showed that the average lake ice cover duration experienced a consistent decreasing for the three regions from 1978-2018. However, in the northern Tibetan Plateau, though the lake ice cover duration showed a shortening trend from 1978 to 2000, it displayed a prolonged trend from 2000 to 2018. Moreover, the air temperature changes of the lake area had a significant correlation with the changes of ice cover duration in each region, and the change of 0 °C isotherm in the Northern Europe lakes are more sensitive than the Mongolian Plateau and the Tibetan Plateau. The air temperature played a major role in the change of lake ice phenology, but there were still other factors that affected the lake ice phenology changes, especially in northern Tibetan Plateau. By comparing the analysis of the ice cover duration in the three regions and the effect of air temperature on the lake ice cover duration change, it provides more evidences for the study on climate change research in different regions. Article in Journal/Newspaper Antarc* Antarctic Climate change IOP Publishing IOP Conference Series: Earth and Environmental Science 502 1 012033
institution Open Polar
collection IOP Publishing
op_collection_id crioppubl
language unknown
description Abstract Lake ice is a sensitive factor for the Earth’s environment and climate change research. In the comparative study on climate change to the Earth three-pole (Antarctic, Arctic, and Tibetan Plateau), the lake ice phenology can be used to represent seasonal climate changes. In this paper, the lake ice phenology and the corresponding daily temperature for 48 lakes in Northern Europe, Tibetan Plateau and Mongolia Plateau were used as the typical case for comparative research. Based on passive microwave remote sensing data. The results showed that the average lake ice cover duration experienced a consistent decreasing for the three regions from 1978-2018. However, in the northern Tibetan Plateau, though the lake ice cover duration showed a shortening trend from 1978 to 2000, it displayed a prolonged trend from 2000 to 2018. Moreover, the air temperature changes of the lake area had a significant correlation with the changes of ice cover duration in each region, and the change of 0 °C isotherm in the Northern Europe lakes are more sensitive than the Mongolian Plateau and the Tibetan Plateau. The air temperature played a major role in the change of lake ice phenology, but there were still other factors that affected the lake ice phenology changes, especially in northern Tibetan Plateau. By comparing the analysis of the ice cover duration in the three regions and the effect of air temperature on the lake ice cover duration change, it provides more evidences for the study on climate change research in different regions.
format Article in Journal/Newspaper
author Xingxing, Wang
Yubao, Qiu
Lemmetyinen, Juha
Pengfei, Xie
Cheng, Bin
Wenshan, Liang
spellingShingle Xingxing, Wang
Yubao, Qiu
Lemmetyinen, Juha
Pengfei, Xie
Cheng, Bin
Wenshan, Liang
Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau
author_facet Xingxing, Wang
Yubao, Qiu
Lemmetyinen, Juha
Pengfei, Xie
Cheng, Bin
Wenshan, Liang
author_sort Xingxing, Wang
title Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau
title_short Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau
title_full Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau
title_fullStr Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau
title_full_unstemmed Comparison to Changes of Lake Ice Phenology and Air Temperature over Northern Europe, Tibetan Plateau and Mongolian Plateau
title_sort comparison to changes of lake ice phenology and air temperature over northern europe, tibetan plateau and mongolian plateau
publisher IOP Publishing
publishDate 2020
url http://dx.doi.org/10.1088/1755-1315/502/1/012033
https://iopscience.iop.org/article/10.1088/1755-1315/502/1/012033/pdf
https://iopscience.iop.org/article/10.1088/1755-1315/502/1/012033
genre Antarc*
Antarctic
Climate change
genre_facet Antarc*
Antarctic
Climate change
op_source IOP Conference Series: Earth and Environmental Science
volume 502, issue 1, page 012033
ISSN 1755-1307 1755-1315
op_rights http://creativecommons.org/licenses/by/3.0/
https://iopscience.iop.org/info/page/text-and-data-mining
op_doi https://doi.org/10.1088/1755-1315/502/1/012033
container_title IOP Conference Series: Earth and Environmental Science
container_volume 502
container_issue 1
container_start_page 012033
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