INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER

章新平, 范钟秀, 周恩济

文章导航 > Chinese Geographical Science > 1994 > 4(1): 31-42

章新平, 范钟秀, 周恩济. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. 中国地理科学, 1994, 4(1): 31-42.

引用本文:

章新平, 范钟秀, 周恩济. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. 中国地理科学, 1994, 4(1): 31-42.

Zhang Xinping, Fan Zhongxiu, Zhou Enji. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. Chinese Geographical Science, 1994, 4(1): 31-42.

Citation:

Zhang Xinping, Fan Zhongxiu, Zhou Enji. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. Chinese Geographical Science, 1994, 4(1): 31-42.

INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER

1.
Lanzhou Institute of Glaciology and Geocryology, the Chinese Academy of Sciences, Lanzhou 730000, PRC;
2.
Hehai University, Nanjing 210024, PRC

INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER

1.
Lanzhou Institute of Glaciology and Geocryology, the Chinese Academy of Sciences, Lanzhou 730000, PRC;
2.
Hehai University. Nanjing 210024, PRC

摘要: On the method of correlation analysis the poper begins with searching the SST (Sea Surface Temperature) and circulation features of some regions with close correlation to the discharge of the flood season (from June to September) in the upper reaches of the Changjiang (Yangtze) River, then discusses the characteristics of sea-air interaction and the relations between the sea-air interaction and the discharge of the flood season, after that analyzes the possible mechanisms through which the main sea regions affect atmospheric circulation, and of the influence of the circulation changes on the discharge of the flood season.
- upper reaches of the Changjiang River /
- discharge of flood season /
- at mospheric circulation /
- sea-air interaction
Abstract: On the method of correlation analysis the poper begins with searching the SST (Sea Surface Temperature) and circulation features of some regions with close correlation to the discharge of the flood season (from June to September) in the upper reaches of the Changjiang (Yangtze) River, then discusses the characteristics of sea-air interaction and the relations between the sea-air interaction and the discharge of the flood season, after that analyzes the possible mechanisms through which the main sea regions affect atmospheric circulation, and of the influence of the circulation changes on the discharge of the flood season.
- upper reaches of the Changjiang River /
- discharge of flood season /
- at mospheric circulation /
- sea-air interaction

[1]	Tian YAO, Qiang ZHAO, Chuanhao WU, Xiaonong HU, Chuan’an XIA, Xuan WANG, Guoqiang SANG, Jian LIU, Haijun WANG. Spatio-temporal Variation Characteristics of Extreme Climate Events and Their Teleconnections to Large-scale Ocean-atmospheric Circulation Patterns in Huaihe River Basin, China During 1959–2019 . Chinese Geographical Science, 2024, 34(1): 118-134. doi: 10.1007/s11769-023-1398-1
[2]	YAN Baixing, GUAN Jiunian, Vladimir SHESTERKIN, ZHU Hui. Variations of Dissolved Iron in the Amur River During an Extreme Flood Event in 2013 . Chinese Geographical Science, 2016, 26(5): 679-686. doi: 10.1007/s11769-016-0828-8
[3]	SHA Yukun, LI Weipeng, FAN Jihui, CHENG Genwei. Determining Critical Support Discharge of a Riverhead and River Network Analysis: Case Studies of Lhasa River and Nyangqu River . Chinese Geographical Science, 2016, 26(4): 456-465. doi: 10.1007/s11769-015-0760-3
[4]	LIU Feng, CHEN Shenliang, PENG Jun, CHEN Guangquan. Temporal Variations of Water Discharge and Sediment Load of Huanghe River, China . Chinese Geographical Science, 2012, 22(5): 507-521.
[5]	ZHANG Lijuan, LIU Dong, YAN Xiaodong et al. Research on analyzing and forecasting the upper air climate change over Harbin . Chinese Geographical Science, 2011, 21(1): 65-73.
[6]	WANG Ning, ZHANG Gang, LIU Te, CAI Qingxiang. Distribution of Methyl Mercury in Rana chensinensis and Environmental Media in Gold-mining Areas of Upper Reaches of Songhua River, China . Chinese Geographical Science, 2010, 20(4): 330-336. doi: 10.1007/s11769-010-0405-5
[7]	WEN Zhaohui, LIN Wantao, LIN Yihua, MO Jiaqi. Dissipative Travelling Wave Solution for El Niño Tropic Sea-air Coupled Oscillator . Chinese Geographical Science, 2010, 20(3): 275-280. doi: 10.1007/s11769-010-0275-x
[8]	CHEN Caocao, XIE Gaodi, ZHEN Lin, LENG Yunfa. Long-term Dynamics of Cultivated Land Resources and Their Driving Forces of Guyuan City in Upper Reaches of Jinghe River . Chinese Geographical Science, 2008, 18(1): 33-40. doi: 10.1007/s11769-008-0033-5
[9]	SHENG Ke-rong, FAN Jie, MA Hai-long. SUSTAINABLE RURAL LIVELIHOOD AND ECOLOGICAL SHELTER CONSTRUCTION IN UPPER REACHES OF CHANGJIANG RIVER——Case Study of Zhaotong of Yunnan Province . Chinese Geographical Science, 2006, 16(1): 32-40.
[10]	MO Jia-qi, LIN Yi-hua, WANG Hui. VARIATIONAL ITERATION SOLVING METHOD FOR SEA-AIR OSCILLATOR MODEL OF INTERDECADAL CLIMATE FLUCTUATIONS . Chinese Geographical Science, 2005, 15(3): 227-230.
[11]	YANG Shi-lun, ZHAO Qing-ying, XIE Wen-hui, WANG Xing-fang. FORECAST OF IMPACTS OF SEA-LEVEL RISE ON THE LOW COLONIZED ISLANDS AND THEIR SURROUNDING WATERS IN THE CHANGJIANG RIVER MOUTH . Chinese Geographical Science, 2000, 10(2): 113-118.
[12]	吕宪国, 张为中. THE FLOOD OF THE NENJIANG RIVER AND THE SONGHUA RIVER IN 1998 AND THE COMPREHENSIVE MANAGEMENT OF THE RIVER BASINS . Chinese Geographical Science, 1999, 9(3): 193-198.
[13]	谭术魁. DEEP THOUGHTS OF LAND UTILIZATION ABOUTTHE RARELY SEVERE FLOODING DISASTERALONG THE MIDDLE AND LOWER REACHES OFTHE CHANGJIANG RIVER IN 1998 . Chinese Geographical Science, 1999, 9(1): 1-11.
[14]	钱步东. PRECIPITATION PATTERNS IN FLOOD SEASON OVER CHINA ASSOCIATED WITH THE EL NI?O/SOUTHERN OSCILlATION . Chinese Geographical Science, 1997, 7(3): 220-228.
[15]	许朋柱. IMPACT OF FUTURE SEA LEVEL RISE ON FLOOD AND WATER LOGGING DISASTERS IN LIXIAHE REGION . Chinese Geographical Science, 1996, 6(1): 35-48.
[16]	林承坤, 高锡珍. EVOLUTION OF RAPIDS OF CREEK MOUTH-BAR AT GEZHOUBA RESERVOIR AND THE IMPACTS ON NAVIGABLE CHANNEL IN THE UPPER REACHES OF THE CHANGJIANG RIVER . Chinese Geographical Science, 1996, 6(3): 223-230.
[17]	季子修, 蒋自巽. IMPACTS OF SEA LEVEL RISE ON COASTAL EROSION IN THE CHANGJIANG RIVER DELTA AND NORTH JIANGSU COASTAL PLAINO . Chinese Geographical Science, 1994, 4(4): 310-321.
[18]	杨桂山. IMPACTS OF FUTURE SEA LEVEL RISE ON SALT WATER INTRUSION IN THE CHANGJIANG RIVER ESTUARY . Chinese Geographical Science, 1992, 2(1): 30-41.
[19]	陈海龙. A STUDY ON REGULARITY OF DROUGHT AND FLOOD IN THE CHANGJIANG RIVER VALLEY DURING LAST 10 CENTURIES . Chinese Geographical Science, 1992, 2(2): 145-158.
[20]	任美锷, 史运良. SEDIMENT DISCHARGE OF THE HUANGHE RIVER AND ITS EFFECT ON SEDIMENTATION OF THE BOHAI SEA AND THE YELLOW SEA . Chinese Geographical Science, 1991, 1(1): 1-18.

WeChat

点击查看大图

计量

文章访问数: 817
HTML全文浏览量: 27
PDF下载量: 854
被引次数: 0

INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER

1. Lanzhou Institute of Glaciology and Geocryology, the Chinese Academy of Sciences, Lanzhou 730000, PRC;

2. Hehai University, Nanjing 210024, PRC

刊出日期: 1994-03-20

关键词:

upper reaches of the Changjiang River /

discharge of flood season /

at mospheric circulation /

sea-air interaction

摘要: On the method of correlation analysis the poper begins with searching the SST (Sea Surface Temperature) and circulation features of some regions with close correlation to the discharge of the flood season (from June to September) in the upper reaches of the Changjiang (Yangtze) River, then discusses the characteristics of sea-air interaction and the relations between the sea-air interaction and the discharge of the flood season, after that analyzes the possible mechanisms through which the main sea regions affect atmospheric circulation, and of the influence of the circulation changes on the discharge of the flood season.

English Abstract

章新平, 范钟秀, 周恩济. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. 中国地理科学, 1994, 4(1): 31-42.

引用本文:

章新平, 范钟秀, 周恩济. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. 中国地理科学, 1994, 4(1): 31-42.

Zhang Xinping, Fan Zhongxiu, Zhou Enji. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. Chinese Geographical Science, 1994, 4(1): 31-42.

Citation:

Zhang Xinping, Fan Zhongxiu, Zhou Enji. INFLUENCE OF SEA-AIR INTERACTION ON THE DISCHARGE OF FLOOD SEASON IN THE UPPER REACHES OF THE CHANGJIANG RIVER[J]. Chinese Geographical Science, 1994, 4(1): 31-42.

全文HTML

/

下载: 全尺寸图片幻灯片

分享

用微信扫码二维码

分享至好友和朋友圈

返回