Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China
Based on the climate factors data and surface vapor pressure (SVP) data of 44 weather stations in Tianshan Mountains during the years 1961-2011, this paper establishes a water vapor content (WVC) estimation model according to the relationship between monthly WVC of radiosonde and corresponding SVP a...
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ftchinacadscimhe:oai:ir.imde.ac.cn:131551/9092 2023-05-15T15:16:30+02:00 Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China HU Wen-feng YAO Jun-qiang HE Qing YANG Qing 2015-05 http://ir.imde.ac.cn/handle/131551/9092 https://doi.org/10.1007/s11629-014-3364-y 英语 eng Journal of Mountain Science HU Wen-feng,YAO Jun-qiang,HE Qing,et al. Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China[J]. Journal of Mountain Science,2015,12(3):571-581. http://ir.imde.ac.cn/handle/131551/9092 doi:10.1007/s11629-014-3364-y cn.org.cspace.api.content.CopyrightPolicy@7e15ed Water Vapor Content Spatial Variability Temporal Variability Microwave Radiometers Tianshan Mountains 期刊论文 2015 ftchinacadscimhe https://doi.org/10.1007/s11629-014-3364-y 2022-12-19T18:19:05Z Based on the climate factors data and surface vapor pressure (SVP) data of 44 weather stations in Tianshan Mountains during the years 1961-2011, this paper establishes a water vapor content (WVC) estimation model according to the relationship between monthly WVC of radiosonde and corresponding SVP and analyzes the spatial and temporal variability of WVC and their causes. The results show that the WVC is linearly and negatively related to the elevation and longitude (Vertical zonality and Longitude zonality), while it was not linearly related to the latitude. The westerly wind, geographical situation and sea level elevation composed complex surface conditions to influence the spatial distribution of WVC in the Tianshan Mountains. The Mann-Kendall (M-K) statistical test shows a significant increasing trend in the mean annual WVC in Tianshan Mountains during 1961-2011(P < 0.001), with a rate of 0.23 mm/decade, and indicates an abrupt turning pointin 1985 (P < 0.001). Correlation analysis shows that the WVC are significantly correlated to the temperature, especially during the winter, but the summer WVC are significantly correlated to the precipitation. In addition, the North Atlantic Oscillation Index (NAOI) and the Arctic Oscillation Index (AOI) are significantly correlated to the winter WVC in the Tianshan Mountains. As a new Microwave radiometric profilers (MWRPs) instrument, the MP-3000A provides continuous, real-time and high temporal resolution atmospheric profiles up to 10 km. In order to monitor water vapor and atmosphere profiles in Tianshan Mountains, an MP-3000A was established in Urumqi (43.8°N, 87.58°N) in May 2008. The results indicated that the MP-3000A was applicable to this area, and the evolutionary process of water vapor and the WVC peak values of MP-3000A were a strong signal for rainstorm and flood forecasts for Urumqi and the Tianshan Mountains. Report Arctic North Atlantic North Atlantic oscillation IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) Arctic Kendall ENVELOPE(-59.828,-59.828,-63.497,-63.497) Journal of Mountain Science 12 3 571 581 |
institution |
Open Polar |
collection |
IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) |
op_collection_id |
ftchinacadscimhe |
language |
English |
topic |
Water Vapor Content Spatial Variability Temporal Variability Microwave Radiometers Tianshan Mountains |
spellingShingle |
Water Vapor Content Spatial Variability Temporal Variability Microwave Radiometers Tianshan Mountains HU Wen-feng YAO Jun-qiang HE Qing YANG Qing Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China |
topic_facet |
Water Vapor Content Spatial Variability Temporal Variability Microwave Radiometers Tianshan Mountains |
description |
Based on the climate factors data and surface vapor pressure (SVP) data of 44 weather stations in Tianshan Mountains during the years 1961-2011, this paper establishes a water vapor content (WVC) estimation model according to the relationship between monthly WVC of radiosonde and corresponding SVP and analyzes the spatial and temporal variability of WVC and their causes. The results show that the WVC is linearly and negatively related to the elevation and longitude (Vertical zonality and Longitude zonality), while it was not linearly related to the latitude. The westerly wind, geographical situation and sea level elevation composed complex surface conditions to influence the spatial distribution of WVC in the Tianshan Mountains. The Mann-Kendall (M-K) statistical test shows a significant increasing trend in the mean annual WVC in Tianshan Mountains during 1961-2011(P < 0.001), with a rate of 0.23 mm/decade, and indicates an abrupt turning pointin 1985 (P < 0.001). Correlation analysis shows that the WVC are significantly correlated to the temperature, especially during the winter, but the summer WVC are significantly correlated to the precipitation. In addition, the North Atlantic Oscillation Index (NAOI) and the Arctic Oscillation Index (AOI) are significantly correlated to the winter WVC in the Tianshan Mountains. As a new Microwave radiometric profilers (MWRPs) instrument, the MP-3000A provides continuous, real-time and high temporal resolution atmospheric profiles up to 10 km. In order to monitor water vapor and atmosphere profiles in Tianshan Mountains, an MP-3000A was established in Urumqi (43.8°N, 87.58°N) in May 2008. The results indicated that the MP-3000A was applicable to this area, and the evolutionary process of water vapor and the WVC peak values of MP-3000A were a strong signal for rainstorm and flood forecasts for Urumqi and the Tianshan Mountains. |
format |
Report |
author |
HU Wen-feng YAO Jun-qiang HE Qing YANG Qing |
author_facet |
HU Wen-feng YAO Jun-qiang HE Qing YANG Qing |
author_sort |
HU Wen-feng |
title |
Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China |
title_short |
Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China |
title_full |
Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China |
title_fullStr |
Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China |
title_full_unstemmed |
Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China |
title_sort |
spatial and temporal variability of water vapor content during 1961 - 2011 in tianshan mountains, china |
publishDate |
2015 |
url |
http://ir.imde.ac.cn/handle/131551/9092 https://doi.org/10.1007/s11629-014-3364-y |
long_lat |
ENVELOPE(-59.828,-59.828,-63.497,-63.497) |
geographic |
Arctic Kendall |
geographic_facet |
Arctic Kendall |
genre |
Arctic North Atlantic North Atlantic oscillation |
genre_facet |
Arctic North Atlantic North Atlantic oscillation |
op_relation |
Journal of Mountain Science HU Wen-feng,YAO Jun-qiang,HE Qing,et al. Spatial and Temporal Variability of Water Vapor Content during 1961 - 2011 in Tianshan Mountains, China[J]. Journal of Mountain Science,2015,12(3):571-581. http://ir.imde.ac.cn/handle/131551/9092 doi:10.1007/s11629-014-3364-y |
op_rights |
cn.org.cspace.api.content.CopyrightPolicy@7e15ed |
op_doi |
https://doi.org/10.1007/s11629-014-3364-y |
container_title |
Journal of Mountain Science |
container_volume |
12 |
container_issue |
3 |
container_start_page |
571 |
op_container_end_page |
581 |
_version_ |
1766346800753541120 |