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大型浅水湖泊高时空分辨率风场特征数值模拟研究:以巢湖为例OACSTPCD

Numerical simulation of wind field characteristics in large shallow lakes with high spatial and temporal resolution:A case study of chaohu lake

中文摘要英文摘要

[目的]大型浅水湖泊的风场是影响湖泊流场、水体富营养化和藻华运移聚集规律的关键因素之一,仅依托气象站点的观测数据难以有效捕捉湖面风场在空间和时间上的快速变化.为精细刻画湖泊高频变化风场,辨识其时空变化特征,[方法]以巢湖为研究对象,综合利用气象观测数据、全球再分析数据集和地理静态数据,通过中尺度天气预报模式和地理空间分析技术,模拟分析巢湖地区2019年高时空分辨率的风场变化过程.[结果]结果显示:巢湖区域风速由东向西、由南向北、由湖面向陆面逐渐减弱;湖面主导风向为东风和偏东风,主导风速为二级至四级,湖面平均风速在11月最大,12月次之,5月最小,不同季节湖面平均风速由大到小依次为冬季、秋季、夏季和春季.[结论]结果表明:巢湖在白天(夜晚)出现冷(暖)湖效应,其风场在早上6时和夜晚23时出现陆风和湖风转换;西半湖受湖陆风和城市热岛影响显著,在夏季会出现明显的环湖湖风锋,其湖风锋穿透内陆距离约4.7~9km;东半湖受山谷风影响显著,在东南部山脉以东湖区易形成低风速区,在湖口附近受狭管效应易形成高风速区.通过研究成果可进一步认知巢湖区域风场特征,为巢湖水生态环境治理提供技术支撑.

[Objective]The wind field of large shallow lakes is one of the key factors affecting the flow field,eutrophication of water and the migration and accumulation of algal blooms.However,it is difficult to effectively capture the rapid changes in space and time of the wind field of the whole lake only relying on the observation data of meteorological stations.[Methods]In order to accurately characterize the high-frequency wind field in the lake and identify its spatio-temporal variation characteristics,the Chaohu Lake was taken as the research object,and the mesoscale weather forecast model and geospatial analysis technology were used to simulate and analyze the wind field variation process with high spatio-temporal resolution in 2019 by comprehensively utilizing meteorological observation data,global reanalysis data and geographic static data.[Results]The result show that,the wind speed in the Chaohu area gradually weakens from east to west,from south to north,and from the lake to the land surface;the dominant wind direction of Chaohu Lake is east wind and easterly wind,and the dominant wind speed ranges from level 2 to level 4.In addition,the average wind speed on the lake surface is the highest in November,followed by December and the lowest in May.The average wind speed on the lake surface in different seasons is winter,autumn,summer and spring in descending order.[Conclusion]Chaohu exhibits a cold(warm)lake effect during the day(night),and its wind field experiences a transi-tion from land breeze to lake breeze at 6 am and 11 pm.At the same time,the western half of the lake is significantly influenced by lake-land breezes and urban heat islands,and a distinct lakefront wind boundary can be observed during the summer,pene-trating inland for about 4.7-9 km.Besides,the eastern half of the lake is significantly affected by the valley breeze,and the low wind speed zone is easy to form in the lake east of the southeastern mountains,and the high wind speed zone is easy to form near the lake mouth due to the funnelling.Through this study,we can further understand the characteristics of Chaohu regional wind field and provide technical support for Chaohu water ecological environment management.

杜飞;孙龙;陈凯麒;刘晓波;王世岩;黄爱平;董飞;刘畅;杜彦良;阳星

流域水循环模拟与调控国家重点实验室,北京 100038||中国水利水电科学研究院,北京 100038

大气科学

巢湖风场湖陆风中尺度天气预报模式气候变化时空变化数值模拟

Chaohu Lakewind fieldlake-land breezemesoscale weather forecasting modelclimate changetemporal and spatial changesnumerical simulation

《水利水电技术(中英文)》 2024 (002)

长江深大水库层化水体的多界面微生物地球化学过程及其环境影响调控研究

39-49 / 11

国家自然科学基金项目(U2040211);国家重点研发计划项目研究课题(2022YFC3201804);三峡后续工作项目(WE1222B112022、WE0161A012023)

10.13928/j.cnki.wrahe.2024.02.004

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