[1]朱 钰,刘时银*,易 颖,等.“三江并流区”水储量的时空变化特征及其对ENSO的响应[J].山地学报,2020,(2):165-179.[doi:10.16089/j.cnki.1008-2786.000499]
　ZHU Yu,LIU Shiyin*,YI Ying,et al.Spatiotemporal Changes of Terrestrial Water Storage in Three Parallel River Basins and Its Response to ENSO[J].Mountain Research,2020,(2):165-179.[doi:10.16089/j.cnki.1008-2786.000499]
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“三江并流区”水储量的时空变化特征及其对ENSO的响应()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2020年第2期
页码:
165-179
栏目:
山地环境
出版日期:
2020-05-10

文章信息/Info

Title:
Spatiotemporal Changes of Terrestrial Water Storage in Three Parallel River Basins and Its Response to ENSO
文章编号:
1008-2786-(2020)2-165-15
作者:
朱 钰1; 2; 刘时银1; 2*; 易 颖1; 2; 李婉秋3; 张思豆1; 2
1.云南大学 国际河流与生态安全研究院,云南 昆明 650091; 2.云南省国际河流与跨境生态重点实验室,云南 昆明 650091; 3.山东科技大学 测绘科学与工程学院,山东 青岛 266590
Author(s):
ZHU Yu1; 2; LIU Shiyin1; 2*; YI Ying1; 2; LI Wanqiu3; ZHANG Sidou1; 2
1. Yunnan Key Laboratory of International Rivers and Transboundary Eco-security, Kunming 650091, Yunnan China; 2. Institute of International Rivers and Eco-Security Yunnan University, Kunming 650091, Yunnan China; 3. College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, Shandong China
关键词:
水储量;  时空分异;  ENSO;  青藏高原;  三江并流区
Keywords:
terrestrial water storage(TWSC);  spatiotemporal differential;  ENSO;  Tibetan Plateau;  Three Parallel Rivers Basin(TPRB)
分类号:
K903
DOI:
10.16089/j.cnki.1008-2786.000499
文献标志码:
A
摘要:
青藏高原东南部的“三江并流区”气候环境复杂且敏感,陆地水循环过程空间分异明显,在全球气候变化背景下,区域旱涝灾害频发,水循环过程发生变化,刻画区域水储量时空变化特征有助于揭示灾害事件产生的原因。本文使用GRACE RL06数据、水文模型数据、实测数据等,反演获得了2002年4月—2016年8月“三江并流区”水储量变化时间序列及其多年变化空间分布,分析了水储量异常与旱涝事件的联系,进一步探讨了ENSO对水储量影响的强度及滞后程度,并就水储量反演的不确定性做了讨论。获得如下结论:(1)区域水储量处于下降状态,除个别年份,水储量的亏损超过35 mm/a,区域整体较干旱,土壤水是水储量变化的主要组分,区域干旱事件的发生大多与土壤水的持续下降有关;(2)水储量变化空间分异明显,西南下降、西北上升,怒江流域为水储量严重亏损的区域,水储量持续下降的区域常伴随着干旱事件的发生;(3)ENSO对水储量变化的影响存在2.72个月的时滞,每个月的影响强度为0.95 mm,水储量存在重大亏损的区域,ENSO影响强度相对偏大;(4)使用双重尺度因子能在一定程度上恢复滤波造成的误差,但受数据空间分辨率的影响,反演结果仍只能反映变化趋势,难以刻画水储量变化的细部特征。
Abstract:
The complex and sensitive climate conditions and natural environment in Three Parallel Rivers Basin(TPRB), located in the southeastern Tibetan Plateau, China, leads to spatial differentiation of terrestrial water cycle. Under the background of climate change, the increasing frequency and intensity of natural disasters, for example, floods and droughts, results in changing of water balance. Therefore, it is necessary to analyze the possible causes of these events through characterizing the change of terrestrial water storage(TWSC). For this purpose, the GRACE RL06 gravity field data, hydrological model data, and measured data were employed to obtain uninterrupted and high-precision TWSC in the TPRB from April 2002 to August 2016. Spatial and temporal differentiation characteristics of TWSC, using different methods, were acquired to qualitatively and quantitatively analyze the response to extreme climate events. Furthermore, the impact of El Niño Southern Oscillation(ENSO)on TWSC was explored, and the uncertainties of TWSC driven by GRACE were discussed. Some findings were shown as follows:(1)There was a downward trend on TWSC in TPRB during study period. Except for individual years, the loss of TWSC was more than 35 mm/a. The main component of TWSC was the change of soil moisture, so it could be inferred occurrence of regional drought events was mostly related to the continuous decline of soil moisture.(2)The spatial differentiation of TWSC was obvious, with a downward trend in the southwest and an upward trend in the northwest. Of the whole study area, Nujiang basin is the area with the largest loss of TWSC. The area where water reserves had declined severely was the area where extreme drought occurs.(3)The influence of ENSO on TWSC exhibted a 2.72 month time lag and an amplitude change of 0.95 mm per month. The influence intensity of ENSO in regions where water reserve showed a significant loss was relatively large.(4)Although the error caused by filtering could be restored to a certain extent by using double-scale factor method, the inversion results, affected by spatial resolution of the data, could only reflect the tendency of TWSC and be of difficulty to describe the detailed characteristics of TWSC.

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备注/Memo

备注/Memo:
收稿日期(Received date):2019-09-30; 改回日期(Accepted date): 2020-03-18
基金项目(Foundation item):云南大学引进人才科研项目(YJRC3201702); 国家自然科学基金国际合作与交流项目(41761144075); 云南大学第十届研究生科研创新项目(2018Z099)。[ Introducing Talent Research Projects In Yunnan University(YJRC3201702); Projects of International Cooperation and Exchange, NSFC(41761144075); The Tenth Graduate Research Innovation Project In Yunnan University(2018Z099)]
作者简介(Biography):朱钰(1992-),男,甘肃平凉人,博士研究生,主要研究方向:水文过程模拟。[ZHU Yu(1992-), male, born in Pingliang, Gansu province. Ph.D. candidate, research on hydrological process simulation] E-mail: yuzhu@mail.ynu.edu.cn
*通讯作者(Corresponding author):刘时银(1963-),男,研究员,主要研究方向:冰冻圈与水循环。[LIU Shiyin(1963-), male, professor, specialized in the cryosphere and water circulation]
更新日期/Last Update: 2020-03-30