台风“海马”对洞庭湖流域降水同位素的影响研究

doi:10.13249/j.cnki.sgs.2019.07.017

地理科学 ›› 2019, Vol. 39 ›› Issue (7): 1184-1190.doi: 10.13249/j.cnki.sgs.2019.07.017

台风“海马”对洞庭湖流域降水同位素的影响研究

黄一民^1,²,赵日梅²,宋献方¹,何清华²,杨柳²,章新平³

^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. 衡阳师范学院城市与旅游学院,湖南衡阳 421002
^3. 湖南师范大学资源与环境科学学院,湖南长沙 410081

收稿日期:2018-12-18 修回日期:2019-02-26 出版日期:2019-07-10 发布日期:2019-07-10
作者简介:黄一民（1980-）,男,湖南汨罗人,博士,讲师,主要从事同位素水文学研究。E-mail: hymin2004@sina.com
基金资助:
湖南省自然科学基金项目(2018JJ2009);湖南省教育厅优秀青年项目(18B370);衡阳师范学院启动项目(17D26);湖南省环境教育研究中心开放基金项目资助(HJ15K03);湖南省环境教育研究中心开放基金项目资助(HJ18K01)

Precipitation Isotopes Formed by Typhoon “Haima” in the Dongting Lake Basin

Huang Yimin^1,²,Zhao Rimei²,Song Xianfang¹,He Qinghua²,Yang Liu²,Zhang Xinping³

^1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Science and Natural Resources Research, Chinese Academy of Science, Beijing 100101, China
^2. City and Tourism Management Department, Hengyang Normal University, Hengyang 421002, Hunan, China
^3. College of Resources and Environmental Sciences, Hunan Normal University, Changsha 410081, Hunan, China

Received:2018-12-18 Revised:2019-02-26 Online:2019-07-10 Published:2019-07-10
Supported by:
Natural Science Foundation of Hunan Province(2018JJ2009);Scientific Research Project of Education Department of Hunan Province for Outstanding Young People(18B370);Scientific Research Startup Project of Hengyang Normal University(17D26);Aid Program of Research Center for Environment Education of Hunan Province(HJ15K03);Aid Program of Research Center for Environment Education of Hunan Province(HJ18K01)

摘要/Abstract

摘要：

基于2011年第4号台风“海马”登陆前后洞庭湖流域内长沙降水同位素资料,分析了降水同位素的变化特征以及水汽输送对降水同位素的影响。结果表明：台风“海马”在洞庭湖流域内长沙所形成降水的大气水线的斜率和截距均小于长沙夏季大气水线,这与根据同位素分馏理论做出的推测相吻合。台风天气系统影响下的流域降水δ ¹⁸O值为研究时段内的最低值,即降水同位素被显著贫化,而降水过量氘（deuterium excess,记为d）波动明显要小于其他时段,后者反映了形成台风降水的水汽来源较为单一。研究时段内长沙降水d指示台风降水前、台风降水中两个阶段水汽来源于西太平洋,水汽输送轨迹也印证了降水d所指示的水汽来源情况,如流域台风降水的水汽主要来自前期台风输送至南海北部的西太平洋水汽。台风降水后这一阶段降水中d指示海洋水汽来源的效果降低,其原因在于海洋水汽输送减少、陆地蒸发旺盛以及下落雨滴蒸发强烈所致。

关键词: 台风, 降水同位素, 洞庭湖流域, 台风“海马”

Abstract:

The variation characteristics of precipitation isotopes and the influence of moisture source on them are analyzed by using precipitation isotope data collected around the No. 4 typhoon, named ‘Haima’, in 2011 at Changsha, which located in the Dongting Lake Basin. The results show that both the slope and the intercept of meteoric water line produced by the typhoon precipitation are smaller than that of summer’s at Changsha, which is consistent with water isotope fractionation theory. Significant deplete in heavy isotopes leads to lowest value of precipitation δ ¹⁸O under the typhoon weather system during the study period, while the deuterium excess(d) is less fluctuation than in the rest time, the latter reflects that the moisture source of the typhoon is relatively single. Precipitation d-excess indicates that moisture is transported from the western Pacific Ocean both before and during the typhoon precipitation, while unclear moisture source after the typhoon precipitation. Also the moisture transport trajectory for precipitation in the basin confirms the moisture sources indicated by precipitation d, for example, the water vapor of typhoon precipitation in the basin mainly comes from the northern South China Sea, and huge water vapor over northern South China Sea had been carried by the typhoon from the western Pacific.

Key words: typhoon, precipitation isotopes, the Dongting Lake Basin, typhoon "Haima"

中图分类号:

P426.2

黄一民,赵日梅,宋献方,何清华,杨柳,章新平. 台风“海马”对洞庭湖流域降水同位素的影响研究[J]. 地理科学, 2019, 39(7): 1184-1190.

Huang Yimin,Zhao Rimei,Song Xianfang,He Qinghua,Yang Liu,Zhang Xinping. Precipitation Isotopes Formed by Typhoon “Haima” in the Dongting Lake Basin[J]. SCIENTIA GEOGRAPHICA SINICA, 2019, 39(7): 1184-1190.

图/表 5

图1

表1

图2

图3

图4

参考文献 31

[1]	Merlivat L, Jouzel J . Global climatic interpretation of the deuterium-oxygen 18 relationship for precipitation[J]. Journal of Geophysical Research, 1979,84:5029-5033.
[2]	Gat J R . Oxygen and hydrogen isotopes in the hydrological cycle[J]. Annual Review of Earth and Planetary Sciences, 1996,24:225-262.
[3]	Jouzel J, Froehlich K, Schotterer U . Deuterium and oxygen-18 in present-day precipitation on data and modelling[J]. Hydrological Sciences, 1997,42(5):747-763.
[4]	Araguás-Araguás L, Froehlich K, Rozanski K . Stable isotope composition of precipitation over southeast Asia[J]. Journal of Geophysical Research, 1998,103(D22):28721-28742.
[5]	孙双峰, 黄建辉, 林光辉 , 等. 稳定同位素技术在植物水分利用研究中的应用[J]. 生态学报, 2005,25(9):2362-2371.
	[ Sun Shuangfeng, Huang Jianhui , Lin Guanghui et al. Application of stable isotope technique in the study of plant water use. Acta Ecologica Sinica, 2005,25(9):2362-2371.]
[6]	黄一民, 孙葭, 黄一斌 , 等基于TES反演数据的亚洲中低纬度地区大气水汽δD的时空分布[J]. 地理学报, 2014,69(11):1661-1672.
	[ Huang Yimin, Sun Jia , Huang Yibin et al. Spatial-temporal distribution of δD in atmospheric water vapor by using TES retrievals over middle to low latitudes in Asia. Acta Geographica Sinica, 2014,69(11):1661-1672.]
[7]	章新平, 施雅风, 姚檀栋 . 青藏高原东北部降水中δ ¹⁸O的变化特征 [J]. 中国科学( B辑), 1995,25(5):540-547.
	[ Zhang Xinping, Shi Yafeng, Yao Tandong . Variation characteristics of δ ¹⁸O in precipitation in the northeast of Qinghai Tibet Plateau . Science in China(Series B), 1995,25(5):540-547.]
[8]	章新平, 姚檀栋 . 影响青藏高原的天气系统与降水中氧同位素的关系[J]. 冰川冻土, 1995,17(2):125-131.
	[ Zhang Xinping, Yao Tandong . Relations between weather systems affecting Tibetan Plateau and oxygen isotope in precipitation. Journal of Glaciology and Geocryology, 1995,17(2):125-131.]
[9]	Guan H, Zhang X , Skrzypek G et al. Deuterium excess variations of rainfall events in a coastal area of south Australia and its relationship with synoptic weather systems and atmospheric moisture sources[J]. Journal of Geophysical Research, 2013,118.
[10]	Bailey H L, Kaufman D S , Henderson A C G et al. Synoptic scale controls on the δ ¹⁸O in precipitation across Beringia [J]. Geophysical Research Letters, 2015,42(11):4608-4616.
[11]	黄一民, 宋献方, 何清华 , 等. 洞庭湖流域下落雨滴蒸发研究[J]. 地理科学, 2018,38(8):169-174.
	[ Huang Yimin, Song Xianfang , He Qinghua et al. Study of sub-cloud evaporation in the Dongting Lake Basin. Scientia Geographica Sinica, 2018,38(8):1364-1369.]
[12]	Fudeyasu H, Ichiyanagi K , Sugimoto A et al. Isotope ratios of precipitation and water vapor observed in Typhoon Shanshan[J]. Journal of Geophysical Research, 2008,113(D12).
[13]	崔江鹏, 田立德, 刘琴 , 等. 青藏高原中部大气水汽稳定同位素捕捉到印度洋台风“费林”信号[J]. 科学通报, 2014,59(35):3526-3532.
	[ Cui Jiangpeng, Tian Lide , Liu Qin et al. Signal of typhoon Phailin from Indian ocean captured by atmospheric water vapor isotope, central Tibetan Plateau(in Chinese). Chin Sci Bull (Chin Ver), 2014,59(35):3526-3532.]
[14]	孙晓双, 王晓艳, 翟水晶 , 等. 台风“麦德姆”福州降水δ ¹⁸O特征及水汽来源分析 [J]. 自然资源学报, 2016,31(6):1041-1050.
	[ Sun Xiaoshuang, Wang Xiaoyan , Zhai Shuijing et al. The analysis of the characteristics and water vapor source of the δ ¹⁸O in the precipitation of typhoon“Matmo”at Fuzhou . Journal of Natural Resources, 2016,31(6):1041-1050.]
[15]	吴华武, 章新平, 关华德 , 等. 不同水汽来源对湖南长沙地区降水中δD、δ ¹⁸O的影响 [J]. 自然资源学报, 2012,27(8):1404-1414. doi: 10.11849/zrzyxb.2012.08.014
	[ Wu Huawu, Zhang Xinping , Guan Huade et al. Influences of different moisture sources on δD and δ ¹⁸O in precipitation in Changsha, Hunan Province . Journal of Natural Resources, 2012,27(8):1404-1414.] doi: 10.11849/zrzyxb.2012.08.014
[16]	Craig H . Isotopic variations in meteoric waters[J]. Science, 1961,133(3465):1702-1703.
[17]	黄一民, 章新平, 孙葭 . 长沙大气水线及与局地气象要素的关系[J]. 长江流域资源与环境, 2014,23(10):1412-1417. doi: 10.11870/cjlyzyyhj201410011
	[ Huang Yimin, Zhang Xinping , Sun Jia et al. Meteoric water line and relationship with local meteorological factors in Changsha. Resources and Environment in the Yangtze Basin, 2014,23(10):1412-1417.] doi: 10.11870/cjlyzyyhj201410011
[18]	Dansgaard W . Stable isotopes in precipitation[J]. Tellus, 1964,16(4):436-468.
[19]	周淑贞 . 气象学与气候学[M]. 北京: 高等教育出版社, 1997.
	[ Zhou Shuzhen. Meteorology and climatology. Beijing: Higher Education Press, 1997.]
[20]	章新平, 张新主, 关华德 , 等. 由TES反演的大气水汽中δD的时空分布特征[J]. 气象学报, 2012,70(6):1367-1380. doi: 10.11676/qxxb2012.115
	[ Zhang Xinping, Zhang Xinzhu , Guan Huade et al. Spatial and temporal distribution characteristics of the δD in the atmospheric vapor as retrieved from the TES data. Acta Meteorologica Sinica, 2012,70(6):1367-1380.] doi: 10.11676/qxxb2012.115
[21]	Brubaker K L, Entekhabi D, Eagleson P S . Estimation of continental precipitation recycling[J]. Journal of Climate, 1993,6(6):1077-1089.
[22]	黄一民, 章新平, 孙葭 , 等. 长沙大气水汽、降水中稳定同位素季节变化及与水汽输送关系[J]. 地理科学, 2015,35(4):498-506.
	[ Huang Yimin, Zhang Xinping , Sun Jia et al. Seasonal variations of stable isotope in precipitation and atmospheric water vapor and their relationship with moisture transportation in Changsha City. Scientia Geographica Sinica, 2015,35(4):498-506.]
[23]	谭明, 南素兰 . 中国季风区降水氧同位素年际变化的“环流效应”初探[J]. 第四纪研究, 2010,30(3):620-622.
	[ Tan Ming, Nan Sulan . Primary investigation on interannual changes in the circulation effect of precipitation oxygen isotopes in monsoon China. Quaternary Sciences, 2010,30(3):620-622.]
[24]	田红, 郭品文, 陆维松 . 中国夏季降水的水汽通道特征及其影响因子分析[J]. 热带气象学报, 2004,20(4):401-408.
	[ Tian Hong, Guo Pinwen, Lu Weisong . Characteristics of vapor inflow corridors related to summer rainfall in China and impact factors. Journal of Tropical Meteorology, 2004,20(4):401-408.]
[25]	Froehlich K, Gibson J J, Aggarwal P K . Deuterium excess in precipitation and its climatological significance. Study of environmental change using isotope techniques[M]. Vienna: International Atomic Energy Agency, 2002.
[26]	田立德, 姚檀栋 , White J W C, 等. 喜马拉雅山中段高过量氘与西风带水汽输送有关[J]. 科学通报, 2005,50(7):669-672. doi: 10.1360/04Td0030
	[ Tian Lide, Yao Tandong , White J W C et al. Westerly moisture transport to the middle of Himalayas revealed from the high deuterium excess. Chinese Science Bulletin, 2005,50(7):669-672.] doi: 10.1360/04Td0030
[27]	章新平, 刘晶淼, 中尾正义 , 等. 我国西南地区降水中过量氘指示水汽来源[J]. 冰川冻土, 2009,31(4):613-619.
	[ Zhang Xinping, Liu Jingmiao , Masayoshi Nakawo et al. Vapor origins revealed by deuterium excess in precipitation in southwest China. Journal of Glaciology and Geocryology, 2009,31(4):613-619.]
[28]	Stewart M K . Stable isotope fractionation due to evaporation and isotopic exchange of falling waterdrops: Applications to atmospheric processes and evaporation of lakes[J]. Journal of Geophysical Research, 1975,80(9):1133-1146.
[29]	Gat J R, Bowser C J, Kendall C . The contribution of evaporation from the Great Lakes to the continental atmosphere: Estimate based on stable isotope data[J]. Geophysical Research Letters, 1994,21(7):557-560.
[30]	谭明, 南素兰, 段武辉 . 中国季风区大气降水同位素的季节尺度环流效应[J]. 第四纪研究, 2016,36(3):575-580. doi: 10.11928/j.issn.1001-7410.2016.03.07
	[ Tan Ming, Nan Sulan, Duan Wuhui . Seasonal scale circulation effect of stable isotope in atmospheric precipitation in the monsoon regions of China. Quaternary Sciences, 2016,36(3):575-580.] doi: 10.11928/j.issn.1001-7410.2016.03.07
[31]	康红文, 谷湘潜, 祝从文 , 等. 我国中部和南部地区降水再循环率评估[J]. 大气科学, 2004,28(6):892-900. doi: 10.3878/j.issn.1006-9895.2004.06.08
	[ Kang Hongwen, Gu Xiangqian , Zhu Congwen et al. Precipitation recycling in southern and central China. Chinese Journal of Atmospheric Sciences, 2004,28(6):892-900.] doi: 10.3878/j.issn.1006-9895.2004.06.08

	δ¹⁸O（‰）			d加权平均（‰）	平均气温（°C）	降水量（mm）	相对湿度(％)
	最小	最大	加权平均	d加权平均（‰）	平均气温（°C）	降水量（mm）	相对湿度(％)
阶段1	-12.6	-4.0	-8.4	12.7	23.5	198.4	91.3
阶段2	-14.3	-8.2	-12.6	11.9	24.9	111.3	92.8
阶段3	-12.3	-5.8	-8.0	9.6	24.9	83.1	89.1

台风“海马”对洞庭湖流域降水同位素的影响研究

Precipitation Isotopes Formed by Typhoon “Haima” in the Dongting Lake Basin

RichHTML

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

图/表 5

参考文献 31

相关文章 12

Metrics

本文评价

推荐阅读 0

[1]	黄一民, 宋献方, 何清华, 章新平. 洞庭湖流域下落雨滴蒸发研究[J]. 地理科学, 2018, 38(8): 1364-1369.
[2]	许红师, 练继建, 宾零陵, 徐奎. 台风灾害多元致灾因子联合分布研究[J]. 地理科学, 2018, 38(12): 2118-2124.
[3]	杨林, 董玉祥, 黄德全, 张雪琴, 杜建会. 海岸沙席形态及近表层沉积物粒度对台风的响应[J]. 地理科学, 2017, 37(8): 1243-1250.
[4]	黄一民, 宋献方, 章新平, 何清华, 韩青, 李强. 洞庭湖流域降水同位素与ENSO关系研究[J]. 地理科学, 2017, 37(5): 792-798.
[5]	黄一民, 宋献方, 章新平, 何清华, 韩青, 凡非得, 贺伟. 洞庭湖流域不同水体中同位素研究[J]. 地理科学, 2016, 36(8): 1252-1260.
[6]	孙葭, 章新平, 黄一民, 张新主. 基于多源降水数据的洞庭湖流域夏季降水与西太平洋副热带高压的关系[J]. 地理科学, 2016, 36(7): 1115-1124.
[7]	周念清, 赵露, 沈新平. 基于Copula函数的洞庭湖流域水沙丰枯遭遇频率分析[J]. 地理科学, 2014, 34(2): 242-248.
[8]	殷洁, 戴尔阜, 吴绍洪. 中国台风灾害综合风险评估与区划[J]. 地理科学, 2013, 33(11): 1370-1376.
[9]	殷杰, 尹占娥, 于大鹏, 许世远. 基于情景的上海台风风暴潮淹没模拟研究[J]. 地理科学, 2013, 33(1): 110-115.
[10]	温家洪, 黄蕙, 陈珂, 叶欣梁, 胡恒智, 华震阳. 基于社区的台风灾害概率风险评估——以上海市杨浦区富禄里居委地区为例[J]. 地理科学, 2012, 32(3): 348-355.
[11]	牛海燕, 刘敏, 陆敏, 权瑞松, 张丽佳, 王静静. 中国沿海地区近20年台风灾害风险评价[J]. 地理科学, 2011, 31(6): 764-768.
[12]	唐晓春, 刘会平, 潘安定, 梁必骐, 李燕彤, 王同美. 广东沿海地区近50年登陆台风灾害特征分析[J]. 地理科学, 2003, 23(2): 182-187.