青藏高原土壤湿度分布特征及其对长江中下游6、7月降水的影响
详细信息 查看官网全文
- 英文论文题名：Distribution of Soil Moisture over the Tibetan Plateau and its effect on the Precipitation in June and July over the Middle and Lower Reaches of Yangtze River Basin
- 论文作者：卓嘎 ; 德吉卓玛 ; 尼玛吉
- 英文论文作者：ZHUO Ga ; DEJI Zhuoma ; NIMA Ji ; Lhasa Branch of Chengdu Institute of Plateau Meteorology ; China Meteorological Administration ; Tibet Climate Center ; Tibet Meteorological Service Center
- 年：2016
- 作者机构：中国气象局成都高原气象研究所拉萨分部;西藏自治区气候中心;西藏自治区气象服务中心;
- 论文关键词：青藏高原 ; 土壤湿度 ; 长江中下游 ; 气候变化
- 英文论文关键词：Tibetan Plateau ; soil moisture ; middle and lower reaches of Yangtze River Basin ; climate change
- 会议召开时间：2016-11-01
- 会议录名称：第33届中国气象学会年会 S3 青藏高原与复杂山地天气气候
- 语种：中文
- 分类号：P461.4
- 学会代码：ZGQX
- 会议名称：第33届中国气象学会年会
- 会议地点：中国陕西西安
- 主办单位：中国气象学会
- 学会名称：中国气象学会
- 页数：13
- 文件大小：3092k
- 原文格式：D
- 会议级别：全国
摘要
采用美国气候预测中心1961-2014年逐月土壤湿度资料以及国家气象信息中心降水格点数据,分析了青藏高原土壤湿度的时空分布特征,以及高原春季土壤湿度对长江中下游6、7月降水的影响。结果表明:青藏高原年和不同季节的土壤湿度空间分布特征基本一致,均呈现从东南向西北减少的趋势。区域平均的土壤湿度显示出高原土壤春季最为干燥,秋季和夏季较为湿润;近50a来青藏高原大部的年、季节土壤湿度均呈略微增加趋势,年、季土壤湿度从20世纪60年代至90年代基本上呈减少,21世纪00年代开始呈缓慢增加趋势。青藏高原春季土壤湿度与长江中下游降水量青藏高原基本呈负相关关系。通过信度检验的负相关区在6月位于高原东北部和西南部,7月位于高原南部,且高原西北部分区域春季土壤湿度和7月降水量存在显著正相关。高原春季土壤湿度通过对高原地表温度的作用,进而影响到高原热力特征、大气环流以及长江中下游降水分布规律。
In order to understand the temporal and spatial distribution of soil moisture over the Tibetan Plateau and its influence on the precipitation in the middle and lower reaches of Yangtze River Basin, with monthly dataset of soil moisture derived from CPC(Climate Prediction Center) and monthly precipitation obtained from NMIC(National Meteorological Information Center) of CMA(Chinese Meteorological Administration) during 1961-2014, the distribution of soil moisture over the Tibetan Plateau has been investigated along with its effect on the precipitation in June and July over the middle and lower reaches of Yangtze River Basin on the basis of correlation analysis. Result shows that seasonal spatial distributions of soil moisture are consistent with the annual distribution and all of them decrease from the southeast part to the northwest part of the Tibetan Plateau. The regional soil moisture presents that it is extremely dry in spring while the moisture is quite humid in autumn and summer over the plateau. Considering the most parts of the plateau, the annual and seasonal soil moistures exhibit slightly increasing trend during the past 50 years. The annual and the seasonal soil moisture basically indicate decreasing trend from 1960 s to 1990 s, and they increase gradually with small magnitude from twenty-first century to the present years. The precipitation in the middle and lower reaches of Yangtze River Basin is negatively related to the spring soil moisture over the plateau on the whole. The negative relation areas which exceed the confidence level are mainly located in the northeast and southwest parts of the plateau in June. The negative areas are situated in the southern plateau while the positive areas are located in the northwest part of the Plateau in July. The spring soil moisture is contributed to the precipitation distribution in the middle and lower reaches of the Yangtze River Basin by means of its effect on the surface temperature, atmospheric circulation and thermal forcing over the Plateau.
In order to understand the temporal and spatial distribution of soil moisture over the Tibetan Plateau and its influence on the precipitation in the middle and lower reaches of Yangtze River Basin, with monthly dataset of soil moisture derived from CPC(Climate Prediction Center) and monthly precipitation obtained from NMIC(National Meteorological Information Center) of CMA(Chinese Meteorological Administration) during 1961-2014, the distribution of soil moisture over the Tibetan Plateau has been investigated along with its effect on the precipitation in June and July over the middle and lower reaches of Yangtze River Basin on the basis of correlation analysis. Result shows that seasonal spatial distributions of soil moisture are consistent with the annual distribution and all of them decrease from the southeast part to the northwest part of the Tibetan Plateau. The regional soil moisture presents that it is extremely dry in spring while the moisture is quite humid in autumn and summer over the plateau. Considering the most parts of the plateau, the annual and seasonal soil moistures exhibit slightly increasing trend during the past 50 years. The annual and the seasonal soil moisture basically indicate decreasing trend from 1960 s to 1990 s, and they increase gradually with small magnitude from twenty-first century to the present years. The precipitation in the middle and lower reaches of Yangtze River Basin is negatively related to the spring soil moisture over the plateau on the whole. The negative relation areas which exceed the confidence level are mainly located in the northeast and southwest parts of the plateau in June. The negative areas are situated in the southern plateau while the positive areas are located in the northwest part of the Plateau in July. The spring soil moisture is contributed to the precipitation distribution in the middle and lower reaches of the Yangtze River Basin by means of its effect on the surface temperature, atmospheric circulation and thermal forcing over the Plateau.
引文
Fan Y,Van Den Dool H.2004.The CPC global monthly soil moisture dataset at 0.5 degree resolution for1948-present[J].Journal of Geophysical Research,109:D10102,doi:10.1029/2003JD004345.
Gao Chujie,Chen Haishan,Xu Bei,et al.2014.Possible relationships among south china sea SSTA,soil moisture anomalies in southwest china and summer precipitation in eastern China[J].Journal of Tropical Meteorology20(3):228-235.
Namias J.1958.Persistence of midtropospheric circulation between adjacent months and seasons[M].Rossby Memorial Volume,Rockefeller Institute press and Oxford University Press,240-248.
Van den Pool H,Huang J,Fan Y.2003.Performance and analysis of the constructed analogue method applied to US soil moisture over 1981-2001[J].Journal of Geophysical Research,108:D168617,doi:10.1029/2002JD003114.
Zhan Yanling,Lin Zhaohui.2011.The relationship between June precipitation over the mid-lower reaches of the Yangtze river basin and spring soil moisture over the east Asian monsoon region[J].Acta Meteorologica Sinica,25(3):355-363.
敖婷,李跃清.2015.夏季青藏高原及周边特例特征与东亚降水的区域关系[J].高原气象,34(5):1204-1216.
陈少勇,郭凯忠,董安祥.2008.黄土高原土壤湿度变化规律研究[J].高原气象,27(3):530-537.
戴长勇,左志燕.2010.中国东部前冬、春土壤湿度与夏季气候的关系[J].气象科技,38(3):300-305.
高楚杰,陈海山,许蓓,等.2013.南海海温和西南地区土壤湿度异常与中国东部夏季降水的可能联系[J].热带气象学报,2013,29(1):75-82.郭东林,杨梅学.2010.SHAW模式对青藏高原中部季节冻土区土壤温、湿度的模拟[J].高原气象,29(6):1369-1377.
姜丽霞,李帅,纪仰慧,等.2009.1980-2005年松嫩平原土壤湿度对气候变化的响应[J].生态学报,2009,20(1):91-97.
李巧萍,丁一汇,董文杰.2007.土壤湿度异常对区域短期气候影响的数值模拟试验[J].应用气象学报,18(1):1-11.Li Qiaoping,Ding Yihui,Dong Wenjie.2007.
梁乐宁,陈海山.2010.春季华南土壤湿度异常与中国夏季降水的可能联系[J].大气科学学报,33(5):536-546.
刘川,余晔,解晋,等.2015.多套土壤温湿度资料在青藏高原的适用性[J].高原气象,34(3):653-665.
刘新,李伟平,许晃雄,等,2007.青藏高原加热对东亚地区夏季降水的影响[J].高原气象,26(6):1287-1292.
马柱国,魏和林,符淙斌.2000.中国东部区域土壤湿度的变化及其与气候变率的关系[J].气象学报,58(3):278-287.
史一丛.2014.土壤湿度-温度初始异常对东亚及周边区域气候模拟的影响[D].南京信息工程大学,硕士论文.
司东,丁一汇,柳艳菊.2010.中国梅雨雨带年代际尺度上的北移及其原因[J].科学通报,55(1):68-73.
王澄海,尚大成.2007.藏北高原土壤温、湿度变化在高原干湿季转换中的作用[J].高原气象,26(4):677-685.
王磊,文军,韦志刚,等.2008.中国西北区西部土壤湿度及其气候响应[J].高原气象,27(6):1257-1266.
王瑞,李伟平,刘新,等.2009.青藏高原春季土壤湿度异常对我国夏季降水影响的模拟研究[J].高原气象,28(6):1233-1241.
王晓婷,郭维栋,钟中,等.2009.中国东部土壤温度、湿度变化的长期趋势及其与气候背景的联系[J].地球科学进展,24(2):181-191.
谢志清,刘晶淼,丁裕国,等.2005.干旱及高寒荒漠区土壤温湿度特征及相互影响的分析[J].高原气象,24(1):16-22.
杨健,马耀明.2012.青藏高原典型下垫面的土壤温湿特征[J].冰川冻土,34(4):813-820.
杨梅学,姚檀栋,丁永建,等.1999.藏北高原D110点不同季节土壤温度的日变化特征[J].地理科学,19(6):570-574.
杨梅学,姚檀栋,Toshio Koike.2000.藏北高原土壤温度的变化特征[J].山地学报,18(1):13-17.
杨梅学,姚檀栋,何元庆.2002.青藏高原土壤水热分布特征及冻融过程在季节转换中的作用[J].山地学报,20(5):553-558.
杨梅学,姚檀栋,王绍令,等.1999.藏北高原土壤温湿特征[J].地理研究,18(3):312-317.
杨梅学,姚檀栋,勾晓华.2000.青藏公路沿线土壤的冻融过程及水热分布特征[J].自然科学进展,10(5):443-450.
姚玉璧,王劲松,王莺,等.2015.黄土高原春季干旱时空分异特征[J].高原气象,34(1):30-38.
岳平,张强,王胜,等.2013.黄土高原半干旱草地降水前后土壤的温、湿度及热力特征[J].中国沙漠,33(6):1766-1774.
张娟,沙占江,徐维新.2015.青藏高原玉树地区巴塘高寒草甸土壤温湿特征分析[J].冰川冻土,37(3):635-642.
张雯,王磊,陈权亮.2015.青藏高原东部土壤湿度变化及其与中国降水的关系[J].成都信息工程学院学报,30(1):81-87.
张镱锂,李炳元,郑度.2003.论青藏高原范围与面积[J].地理研究,21(1):1-8.
詹艳玲,林朝晖.2010.6月长江中下游降水和春季东亚季风区土壤湿度的关系[J].气象学报,70(2):236-243.
赵逸舟,马耀明,马伟强,等.2007.藏北高原土壤温湿变化特征分析[J].冰川冻土,29(4):578-583.
朱晨,师春香,席琳,等.2013.中国区域不同深度土壤湿度模拟和评估[J].气象科技,41(3):529-536.
左志燕,张人禾.2007.中国东部夏季降水与春季土壤湿度的联系[J].科学通报,54(14):1722-1724.
左志燕,张人禾.2008.中国东部春季土壤湿度的时空变化特征[J].中国科学D辑:地球科学,38(11):1428-1437.
Gao Chujie,Chen Haishan,Xu Bei,et al.2014.Possible relationships among south china sea SSTA,soil moisture anomalies in southwest china and summer precipitation in eastern China[J].Journal of Tropical Meteorology20(3):228-235.
Namias J.1958.Persistence of midtropospheric circulation between adjacent months and seasons[M].Rossby Memorial Volume,Rockefeller Institute press and Oxford University Press,240-248.
Van den Pool H,Huang J,Fan Y.2003.Performance and analysis of the constructed analogue method applied to US soil moisture over 1981-2001[J].Journal of Geophysical Research,108:D168617,doi:10.1029/2002JD003114.
Zhan Yanling,Lin Zhaohui.2011.The relationship between June precipitation over the mid-lower reaches of the Yangtze river basin and spring soil moisture over the east Asian monsoon region[J].Acta Meteorologica Sinica,25(3):355-363.
敖婷,李跃清.2015.夏季青藏高原及周边特例特征与东亚降水的区域关系[J].高原气象,34(5):1204-1216.
陈少勇,郭凯忠,董安祥.2008.黄土高原土壤湿度变化规律研究[J].高原气象,27(3):530-537.
戴长勇,左志燕.2010.中国东部前冬、春土壤湿度与夏季气候的关系[J].气象科技,38(3):300-305.
高楚杰,陈海山,许蓓,等.2013.南海海温和西南地区土壤湿度异常与中国东部夏季降水的可能联系[J].热带气象学报,2013,29(1):75-82.郭东林,杨梅学.2010.SHAW模式对青藏高原中部季节冻土区土壤温、湿度的模拟[J].高原气象,29(6):1369-1377.
姜丽霞,李帅,纪仰慧,等.2009.1980-2005年松嫩平原土壤湿度对气候变化的响应[J].生态学报,2009,20(1):91-97.
李巧萍,丁一汇,董文杰.2007.土壤湿度异常对区域短期气候影响的数值模拟试验[J].应用气象学报,18(1):1-11.Li Qiaoping,Ding Yihui,Dong Wenjie.2007.
梁乐宁,陈海山.2010.春季华南土壤湿度异常与中国夏季降水的可能联系[J].大气科学学报,33(5):536-546.
刘川,余晔,解晋,等.2015.多套土壤温湿度资料在青藏高原的适用性[J].高原气象,34(3):653-665.
刘新,李伟平,许晃雄,等,2007.青藏高原加热对东亚地区夏季降水的影响[J].高原气象,26(6):1287-1292.
马柱国,魏和林,符淙斌.2000.中国东部区域土壤湿度的变化及其与气候变率的关系[J].气象学报,58(3):278-287.
史一丛.2014.土壤湿度-温度初始异常对东亚及周边区域气候模拟的影响[D].南京信息工程大学,硕士论文.
司东,丁一汇,柳艳菊.2010.中国梅雨雨带年代际尺度上的北移及其原因[J].科学通报,55(1):68-73.
王澄海,尚大成.2007.藏北高原土壤温、湿度变化在高原干湿季转换中的作用[J].高原气象,26(4):677-685.
王磊,文军,韦志刚,等.2008.中国西北区西部土壤湿度及其气候响应[J].高原气象,27(6):1257-1266.
王瑞,李伟平,刘新,等.2009.青藏高原春季土壤湿度异常对我国夏季降水影响的模拟研究[J].高原气象,28(6):1233-1241.
王晓婷,郭维栋,钟中,等.2009.中国东部土壤温度、湿度变化的长期趋势及其与气候背景的联系[J].地球科学进展,24(2):181-191.
谢志清,刘晶淼,丁裕国,等.2005.干旱及高寒荒漠区土壤温湿度特征及相互影响的分析[J].高原气象,24(1):16-22.
杨健,马耀明.2012.青藏高原典型下垫面的土壤温湿特征[J].冰川冻土,34(4):813-820.
杨梅学,姚檀栋,丁永建,等.1999.藏北高原D110点不同季节土壤温度的日变化特征[J].地理科学,19(6):570-574.
杨梅学,姚檀栋,Toshio Koike.2000.藏北高原土壤温度的变化特征[J].山地学报,18(1):13-17.
杨梅学,姚檀栋,何元庆.2002.青藏高原土壤水热分布特征及冻融过程在季节转换中的作用[J].山地学报,20(5):553-558.
杨梅学,姚檀栋,王绍令,等.1999.藏北高原土壤温湿特征[J].地理研究,18(3):312-317.
杨梅学,姚檀栋,勾晓华.2000.青藏公路沿线土壤的冻融过程及水热分布特征[J].自然科学进展,10(5):443-450.
姚玉璧,王劲松,王莺,等.2015.黄土高原春季干旱时空分异特征[J].高原气象,34(1):30-38.
岳平,张强,王胜,等.2013.黄土高原半干旱草地降水前后土壤的温、湿度及热力特征[J].中国沙漠,33(6):1766-1774.
张娟,沙占江,徐维新.2015.青藏高原玉树地区巴塘高寒草甸土壤温湿特征分析[J].冰川冻土,37(3):635-642.
张雯,王磊,陈权亮.2015.青藏高原东部土壤湿度变化及其与中国降水的关系[J].成都信息工程学院学报,30(1):81-87.
张镱锂,李炳元,郑度.2003.论青藏高原范围与面积[J].地理研究,21(1):1-8.
詹艳玲,林朝晖.2010.6月长江中下游降水和春季东亚季风区土壤湿度的关系[J].气象学报,70(2):236-243.
赵逸舟,马耀明,马伟强,等.2007.藏北高原土壤温湿变化特征分析[J].冰川冻土,29(4):578-583.
朱晨,师春香,席琳,等.2013.中国区域不同深度土壤湿度模拟和评估[J].气象科技,41(3):529-536.
左志燕,张人禾.2007.中国东部夏季降水与春季土壤湿度的联系[J].科学通报,54(14):1722-1724.
左志燕,张人禾.2008.中国东部春季土壤湿度的时空变化特征[J].中国科学D辑:地球科学,38(11):1428-1437.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |