气候变化研究进展 ›› 2021, Vol. 17 ›› Issue (3): 352-360.doi: 10.12006/j.issn.1673-1719.2020.042
尚华明1(), 范煜婷1, 张瑞波1, 喻树龙1, 张同文1, 魏文寿1, 刘卫平2
收稿日期:
2020-03-05
修回日期:
2020-04-20
出版日期:
2021-05-30
发布日期:
2021-06-01
作者简介:
尚华明,男,副研究员, 基金资助:
SHANG Hua-Ming1(), FAN Yu-Ting1, ZHANG Rui-Bo1, YU Shu-Long1, ZHANG Tong-Wen1, WEI Wen-Shou1, Liu Wei-Ping2
Received:
2020-03-05
Revised:
2020-04-20
Online:
2021-05-30
Published:
2021-06-01
摘要:
水资源是制约中国西北干旱区社会经济可持续发展和生态安全的关键因素。以发源于帕米尔高原东部的喀什噶尔河和叶尔羌河流域为研究区,基于该区6个气象站月平均气温和降水量观测资料,以及5条代表性河流的出山口水文站1950年代晚期以来的月径流量观测数据,分析了该区域气候和水文年际变化特征,以及气候变化背景下径流量的响应特征。结果发现:(1)研究区降水、气温都呈显著上升趋势,除盖孜河外,所有河流径流量均呈显著上升趋势。河流径流量的年内分布和年际变化特征反映了各河流径流主要补给来源的差异。(2)帕米尔高原东部河流出山口径流量受到气温和降水的共同影响,其中以冰川补给为主的叶尔羌河、库山河和盖孜河年径流量与当年夏季(6—8月)气温显著正相关(P<0.001);以降水和积雪补给为主的提孜那甫河和克孜河年径流量与上年7月至当年6月降水量显著正相关(P<0.001)。(3)随着气温升高和降水量增加,流域的蒸发加剧,帕米尔高原东部河流径流量对气候变化的响应出现了明显的变化:年径流量与夏季气温的正相关关系减弱,与上年7月至当年6月降水量正相关增强。
尚华明, 范煜婷, 张瑞波, 喻树龙, 张同文, 魏文寿, 刘卫平. 帕米尔高原东部径流量变化及其对气候变化的响应[J]. 气候变化研究进展, 2021, 17(3): 352-360.
SHANG Hua-Ming, FAN Yu-Ting, ZHANG Rui-Bo, YU Shu-Long, ZHANG Tong-Wen, WEI Wen-Shou, Liu Wei-Ping. Streamflow variation in the eastern Pamirs and its response to climate change[J]. Climate Change Research, 2021, 17(3): 352-360.
图5 帕米尔高原东部年径流量与流域逐月气温和降水量的相关系数 注:横坐标P表示上一年,C表示当年,数字代表月份。
Fig. 5 Correlation coefficients between annual streamflow and monthly temperature, precipitation from May in the previous year to December
图6 帕米尔高原东部河流年径流量与气温(6—8月)和降水量(上年7月至当年6月)的滑动相关变化
Fig. 6 Correlation coefficients with the 21-year moving window between annual streamflow and temperature and precipitationin the eastern Pamirs
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