论我国夏季风影响过渡区及其陆—气相互作用问题

doi:10.11867/j.issn.1001-8166.2017.10.1009

地球科学进展 ›› 2017, Vol. 32 ›› Issue (10): 1009 -1019. doi: 10.11867/j.issn.1001-8166.2017.10.1009

张强 ^1, ^2, ³(

), 张红丽 ^1, ^3, ^*(

), 张良 ^1, ², 岳平 ^1, ^2, ³

1.中国气象局兰州干旱气象研究所/甘肃省干旱气候变化与减灾重点实验室/中国气象局干旱气候变化与减灾重点开放实验室,甘肃兰州 730020
2.甘肃省气象局,甘肃兰州 730020
3.兰州大学大气科学学院, 甘肃兰州 730000

收稿日期:2017-07-28 修回日期:2017-09-01 出版日期:2017-12-20
通讯作者: 张红丽 E-mail:zhangqiang@cma.gov.cn;zhanghl13@lzu.edu.cn
基金资助:
国家自然科学基金重点项目“我国典型夏季风影响过渡区陆—气相互作用及其对夏季风响应研究”(编号:41630426)资助.

Study on Summer Monsoon Transition Zone and Its Land-Air Interaction

Qiang Zhang ^1, ^2, ³( ), Hongli Zhang ^1, ^3, ^*( ), Liang Zhang ^1, ², Ping Yue ^1, ^2, ³

1.Institute of Arid Meteorology, China Meteorological Administration, Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province; Key Open Laboratory of Arid Climatic Change and Disaster Reduction of CMA, Lanzhou 730020, China
2.Gansu Provincial Meteorological Bureau, Lanzhou 730020, China
3.College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China

Received:2017-07-28 Revised:2017-09-01 Online:2017-12-20 Published:2017-10-20
Contact: Hongli Zhang E-mail:zhangqiang@cma.gov.cn;zhanghl13@lzu.edu.cn
About author:
First author:Zhang Qiang(1965-),male,Jingyuan County, Gansu Province, Professor. Resaearch areas include atmospheric boundary layer,landsurface process and arid climate.E-mail:zhangqiang@cma.gov.cn
Supported by:
Project supported by the National Natural Science Foundation of China “Study on interaction between land-atmosphere over Typical Summer Monsoon Edgy region and its response to summer monson characteristics”(No.41630426).

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我国季风影响过渡区既是典型的生态过渡区和生态环境脆弱带,也是我国干旱和水土流失最为严重的区域,其陆—气相互作用在天气气候演变过程中扮演着重要角色,所以该特殊区域陆—气相互作用研究是一个重要的科学问题。为此,国家自然科学基金重点资助“我国典型夏季风影响过渡区陆—气相互作用及其对夏季风响应研究”课题专门针对此问题开展研究。在归纳我国夏季风活动的特点、夏季风影响过渡区的形成及其气候环境特征的基础上,总结了目前夏季风影响过渡区及其陆—气相互作用研究进展,综合分析了该地区陆—气相互作用的特殊性。并且提出了该领域研究存在的主要科学问题及未来的研究方向。这对今后深入研究我国夏季风影响过渡区陆—气相互作用问题具有科学指导意义。

关键词: 夏季风影响过渡区, 陆—气相互作用, 夏季风

The Summer Monsoon Transition Zone is a typical area, which is a transitional zone and has a fragile ecological environment. The area also has the most serious drought and soil erosion disaster. Its land-air interaction plays an important role on evolution of weather and climate, and research on land-air interaction in this zone is an important scientific problems. Therefore, a key project, “land-air interaction of the typical summer monsoon transition zone and its response to the summer monsoon”, by National Natural Science Foundation of China aims at this problem. This study summarized the advances about current summer monsoon transition zone and its land-air interaction. Then, based on the characteristics of summer monsoon activities, the formation of this typical area, its advances of climate and environment characteristics were concluded. Peculiarity of land-air interaction in the area was also analyzed comprehensively. Furthermore, the main problems and direction of scientific research in this field are brought forward. It will have scientific guiding significance for in-depth study of land-air interaction in summer monsoon transition zone in future.

Key words: Summer monsoon transition zone, Land-air interaction, Monsoon.

中图分类号:

P404

图1 气候平均的气象要素逐侯变化(据参考文献[9]改绘)
(a)假相当位温( T>340 K);(b)标准化可降水量( P>0.618);(c)西南风( u>0 m/s, v>2 m/s);(d)东南风( u<0 m/s, v>2 m/s)

Fig.1 Pentad change of meteorological elements(modified after reference[9])
(a)Pseudoe quivalent potential temperature( T>340 K); (b)Standardized precipitation( P>0.618); (c)Southwest winds ( u>0 m/s, v>2 m/s) and (d) Southeast winds( u<0 m/s, v>2 m/s)

图2 不同经度季风北边缘的年际波动方差(据参考文献[9]改绘)

Fig.2 Interannual fluctutation variance of northernmost margin of the Asian Summer monsoon in different longitude(modified after reference[9])

图3 夏季风影响过渡区的分布特征(据参考文献[9]改绘)
色标表示气候干燥度

Fig.3 Distribution of summer monsoon transition zone (modified after reference[9])
Color bar is dry degree

图4 夏季(a)平均降水量(据参考文献[11]改绘,单位:mm)和(b)鲍恩比 ^{[

17
]}(单位:1)的水平空间分布

Fig.4 The spatial distribution of average rainfall in summer (a) (modified after reference[11], unit: mm) and Bowen ratio ^{[

17
]} (b) (unit: 1)

图5 季风影响过渡区(a)生态植被(引自中国科学院资源环境科学数据中心)和(b)潜在蒸发量(据参考文献[19]改绘)空间分布特征

Fig.5 The distribution of (a)vegetation (citation from Resources and Environment Science Data Center,Chinese Academy of Sciences) and (b) potential evapotranspiration(modified after reference[19]) in summer monsoon transition zone

图6 夏季风影响过渡区夏季晴天对流层边界层厚度(a)和陆面感热通量日最大值(b)由西向东的降低趋势(据参考文献[4]改绘)

Fig.6 The reducing trend of sunny summer tropospheric boundary layer thickness (a) and the maximum land surface sensible heat flux (b) (modified after reference[4]) in summer monsoon transition zone

图7 夏季风驱动下区域气候与陆面过程和边界层过程之间相互作用的基本物理框架

Fig.7 The basic physics frameworks of interaction between regional climate and processes of land surface and boundary layer

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