Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements

Permafrost conditions in mountain ranges are sensitive to regional land surface temperature (LST), among other factors. To explore that relationship, this study carried out 3 steps: (1) validated Moderate Resolution Imaging Spectroradiometer 1-km daily LST data using data measured in situ, (2) used...

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Main Authors: Zhandong Sun, Hongxiu Wan, Stephan Imbery, Tom Lotz, Lorenz King
Format: Article
Language:English
Published: International Mountain Society 2015-11-01
Series:Mountain Research and Development
Subjects:
Online Access:http://www.bioone.org/doi/full/10.1659/MRD-JOURNAL-D-14-00001.1
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spelling doaj-c43552adebed4496b0546bf21c35ad382020-11-25T00:33:48ZengInternational Mountain SocietyMountain Research and Development0276-47411994-71512015-11-0135432833710.1659/MRD-JOURNAL-D-14-00001.1Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ MeasurementsZhandong Sun0Hongxiu Wan1Stephan Imbery2Tom Lotz3Lorenz King4State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China; Key Laboratory of Watershed Geographic Sciences, Chinese Academy of Sciences, Nanjing, China; sun@niglas.ac.cnState Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China; International Institute for Earth System Science, Nanjing University, Nanjing, ChinaDepartment of Geography, Justus Liebig University Giessen, Giessen, GermanyState Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, ChinaDepartment of Geography, Justus Liebig University Giessen, Giessen, GermanyPermafrost conditions in mountain ranges are sensitive to regional land surface temperature (LST), among other factors. To explore that relationship, this study carried out 3 steps: (1) validated Moderate Resolution Imaging Spectroradiometer 1-km daily LST data using data measured in situ, (2) used the Harmonic Analysis of Time Series (HANTS) algorithm for fitting and removing the influence of clouds, and (3) analyzed the spatial and temporal characteristics of LST dynamics in the central Tien Shan mountain range based on remote-sensing data improved by covariance and empirical orthogonal function analysis. The results indicate that the in situ data present a basic reference for rebuilding invalid values in the retrieved data, and the data gap in daily LST products can be logically reconstructed with the HANTS algorithm. Major long-term and large-scale patterns can be well extracted with the reconstructed LST data. The most dynamic and sensitive LST areas occurred in the buffers around the periglacial areas. Areas above the periglacial line mainly exhibited a decrease in LST, while areas below it showed an increase. This suggests that the periglacial line of the central Tien Shan region has risen during the past decade. These findings can provide a reference for how periglacial areas respond to climate change and how this may affect hydrological and ecological processes.http://www.bioone.org/doi/full/10.1659/MRD-JOURNAL-D-14-00001.1land surface temperature (LST)permafrostHANTS algorithmspatiotemporal patternscentral Tien Shan Mountains
collection DOAJ
language English
format Article
sources DOAJ
author Zhandong Sun
Hongxiu Wan
Stephan Imbery
Tom Lotz
Lorenz King
spellingShingle Zhandong Sun
Hongxiu Wan
Stephan Imbery
Tom Lotz
Lorenz King
Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements
Mountain Research and Development
land surface temperature (LST)
permafrost
HANTS algorithm
spatiotemporal patterns
central Tien Shan Mountains
author_facet Zhandong Sun
Hongxiu Wan
Stephan Imbery
Tom Lotz
Lorenz King
author_sort Zhandong Sun
title Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements
title_short Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements
title_full Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements
title_fullStr Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements
title_full_unstemmed Dynamics of Land Surface Temperature in the Central Tien Shan Mountains: Analysis Based on RS Retrieved Data Validated With In Situ Measurements
title_sort dynamics of land surface temperature in the central tien shan mountains: analysis based on rs retrieved data validated with in situ measurements
publisher International Mountain Society
series Mountain Research and Development
issn 0276-4741
1994-7151
publishDate 2015-11-01
description Permafrost conditions in mountain ranges are sensitive to regional land surface temperature (LST), among other factors. To explore that relationship, this study carried out 3 steps: (1) validated Moderate Resolution Imaging Spectroradiometer 1-km daily LST data using data measured in situ, (2) used the Harmonic Analysis of Time Series (HANTS) algorithm for fitting and removing the influence of clouds, and (3) analyzed the spatial and temporal characteristics of LST dynamics in the central Tien Shan mountain range based on remote-sensing data improved by covariance and empirical orthogonal function analysis. The results indicate that the in situ data present a basic reference for rebuilding invalid values in the retrieved data, and the data gap in daily LST products can be logically reconstructed with the HANTS algorithm. Major long-term and large-scale patterns can be well extracted with the reconstructed LST data. The most dynamic and sensitive LST areas occurred in the buffers around the periglacial areas. Areas above the periglacial line mainly exhibited a decrease in LST, while areas below it showed an increase. This suggests that the periglacial line of the central Tien Shan region has risen during the past decade. These findings can provide a reference for how periglacial areas respond to climate change and how this may affect hydrological and ecological processes.
topic land surface temperature (LST)
permafrost
HANTS algorithm
spatiotemporal patterns
central Tien Shan Mountains
url http://www.bioone.org/doi/full/10.1659/MRD-JOURNAL-D-14-00001.1
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