[1]王飞宇,占车生*,贾仰文,等.不同土壤湿度资料在太行山区的对比[J].山地学报,2016,(03):257-265.[doi:10.16089/j.cnki.1008-2786.000126]
 WANG Feiyu,ZHAN Chesheng,JIA Yangwen,et al.Comparison of Different Soil Moisture Recorcls in the Taihang Mountains, China[J].Mountain Research,2016,(03):257-265.[doi:10.16089/j.cnki.1008-2786.000126]
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不同土壤湿度资料在太行山区的对比()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年03期
页码:
257-265
栏目:
山地生态和环境
出版日期:
2016-06-01

文章信息/Info

Title:
Comparison of Different Soil Moisture Recorcls in the Taihang Mountains, China
文章编号:
1008-2786-(2016)3-257-09
作者:
王飞宇12占车生1*贾仰文3牛存稳3胡 实1
1.中国科学院地理科学与资源研究所/陆地水循环及地表过程重点实验室, 北京 100101;
2.中国科学院大学, 北京 100049;
3.中国水利水电科学研究院/流域水循环模拟与调控国家重点实验室, 北京100038
Author(s):
WANG Feiyu12 ZHAN Chesheng1 JIA Yangwen3 NIU Cunwen3 HU Shi1
1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China;
3. State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin,China Institute of Water Resources and Hydropower Research, Beijing 100038, China
关键词:
土壤湿度 太行山 再分析数据 资料对比
Keywords:
Taihang Mountain soil moisture reanalysis data data comparison
分类号:
S152.7
DOI:
10.16089/j.cnki.1008-2786.000126
文献标志码:
A
摘要:
利用高时空分辨率地面气象数据驱动陆面模式CLM3.5得到的土壤湿度资料,结合ERA40和NCEP-2再分析资料,系统对比分析了1980—2008年太行山区生长季(5—9月)表层(0~10 cm)土壤湿度时空变化,并利用站点观测资料(1993—2008年)对三套资料在太行山区的适应性进行了验证和比较。结果表明:CLM3.5资料和ERA40资料能较好地描述太行山区土壤湿度的年际和年内变化特征,且两者的土壤湿度呈现相对一致的“北干南湿”格局,其中CLM3.5资料土壤湿度的时空变率高于ERA40资料; 而NCEP-2资料对土壤湿度时空分布的描述效果较差。太行山区土壤湿度与降水和相对湿度呈显著的正相关,与气温呈显著的负相关,实际条件下土壤湿度与气候变化的相互作用机制更加复杂。
Abstract:
A sets of soil moisture data produced from CLM3.5 driven by the China Meteorological Forcing Dataset, and two widely-used re-analysis soil moisture datasets(ERA40 and NCEP-2)were used to systematically and comparably analyze the spatial-temporal variations of surface(0~10 cm)soil moisture in the growing season(May to September)over the Taihang Mountains from 1980 to 2008, and matched them with observational data within the same study area. Results show that CLM3.5 data and ERA40 data are generally consistent well with the observations, and both exhibits a relatively consistency of spatial distribution of soil moisture,namely dry in the north while wet in the south, in which spatio-temporal variability of soil moisture simulated by CLM3.5 is larger than that of ERA40 data. However, NCEP-2 doesn't describe the spatio-temporal distribution of soil moisture well. Moreover, soil moisture has significantly positive correlation with precipitation and relative humidity in the Taihang Mountains,wheraes negative correlation with air temperature. In real condition, the mechanism of interaction between soil moisture and climate change is more complex.

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备注/Memo

备注/Memo:
收稿日期(Received date):2015-10-06; 改回日期(Accepted):2015-11-16。
基金项目(Foundation item):国家重点基础研究发展计划(2015CB452701),国家自然科学基金项目(41571019,51209224, 41271003)资助。[Supported by National Key Basic Research Development Program of China(973Program), No. 2015CB452701; National Natural Science Foundation of China, No. 41571019, 51209224 and 41271003.]
作者简介(Biography):王飞宇(1992-), 女, 陕西西安人, 硕士, 主要从事流域水循环模拟研究。[Wang Feiyu(1992-), female, born in Xi'an, Shannxi, Master candidate, major in water cycle simulation.] E-mail: wangfy.14s@igsnrr.ac.cn
*通信作者(Corresponding author):占车生(1975-)。[Zhan Chesheng(1975-)] E-mail: zhancs@igsnrr.ac.cn
更新日期/Last Update: 2016-05-30