首页|期刊导航|中国水利水电科学研究院学报(中英文)|云南高原异龙湖冬季典型日湖面风场特征及其形成机制

云南高原异龙湖冬季典型日湖面风场特征及其形成机制OA

Characteristics of the wind field over plateau lakes in Yunnan Province on a typical winter day and its formation mechanisms

中文摘要英文摘要

湖面风场在驱动大型湖泊湖流、影响湖内污染物输运等方面起着重要作用,湖面风边界条件不准确是影响湖泊水动力水质模型可靠性的重要原因.当前对高原湖泊湖面风场特征、形成机制等方面的认识还不够深入,进而影响了对高原湖泊湖流的认识,对高原湖泊生态环境治理和保护形成了制约.本文以云南异龙湖作为高原湖泊的代表,利用中尺度气候模式WRF_CLM模拟了异龙湖湖盆在冬季典型日的局地气候特征,讨论了湖面风场的特征及形成机制,结果表明:异龙湖湖盆内风场受高空背景风场、湖陆风、湖周地形乃至湖边城市热岛的共同影响,热力在湖面风场形成中的作用不可忽视;湖盆内存在明显的湖陆风,其中湖风时段为11时至16时,陆风时段为18时至次日10时;湖风影响陆面高度范围为一般不超过湖面以上100~300 m;高空背景风场一般仅在湖风时段对陆面风场影响较为明显,但对湖面风场影响不大,在陆风时段对陆面及湖面风场的影响均不明显;来风方向的高大山体及近湖山体在塑造湖面风场方面有一定的作用;湖面风场具有明显的空间不均匀性,在湖周乃至湖面的单点或少数点的风力风向观测结果不足以较好地描述湖面真实风场.

The wind field over the lake surface plays a crucial role in driving lake flows and influencing the trans-port of pollutants within the lake.The inaccurate boundary condition for the lake surface wind is an important reason affecting the reliability of hydrodynamic and water quality models of lakes.The current understanding of the charac-teristics and the formation mechanism of the wind field over plateau lakes is still insufficient,which in turn affects our understanding of lake flows and imposes constraints on the governance and protection of plateau lake ecological systems.This study takes the Yilong Lake,one of the nine major plateau lakes in Yunnan,as a representative.It employs the mesoscale meteorological model WRF_CLM to simulate the local climatic characteristics of the Yilong Lake basin on a typical winter day and discusses the characteristics and formation mechanisms of the lake surface wind field.The results indicate that the wind field within the Yilong Lake basin during the study period is influ-enced by a combination of upper-level background winds,lake-land breezes,surrounding topography,and the urban heat island near the lake;Thermal dynamics play an indispensable role in the formation of the wind field over the lake surface;There is a distinct lake-land breeze in the basin,with lake breezes occurring between 11:00 and 16:00 and land breezes between 18:00 and 10:00 the following day.The area influenced by lake breezes typically spans around the lake within the range less than 100~300 meters above the lake surface.During the lake breeze pe-riod,the upper-level background wind generally has a marked impact on the land surface wind field,but its effect on the lake surface wind field is limited.During the land breeze period,the influences on both the land and lake surface wind fields are not significant.Additionally,tall mountains in the wind direction and nearby hills also play a role in shaping the lake surface wind field.The lake surface wind field exhibits notable spatial heterogeneity,which suggests that measurements of wind speed and direction from single or few points around the lake or on its sur-face are insufficient to accurately represent the true wind field over the lake.

张达;冯顺新;郭红民;马巍

中国水利水电科学研究院,北京 100038||三峡大学,湖北宜昌 443002中国水利水电科学研究院,北京 100038三峡大学,湖北宜昌 443002中国水利水电科学研究院,北京 100038

天文与地球科学

中尺度气候模式风场高原湖泊异龙湖湖陆风

mesoscale climate modelwind fieldplateau lakethe Yilong Lakelake-land breeze

《中国水利水电科学研究院学报(中英文)》 2026 (1)

47-64,18

云南省滇中引水工程有限公司项目(DZYS-ZH-HJBH-SJ-003)

10.13244/j.cnki.jiwhr.20240215

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