| 太湖湖表反照率时空特征及影响因子 |
| 摘要点击 1635 全文点击 1067 投稿时间：2014-06-05 修订日期：2015-05-05 |
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| 中文关键词 反照率 晴空指数 云量 风速 浊度 叶绿素a |
| 英文关键词 albedo clearness index cloudiness wind speed turbidity chlorophyll-a |
| 作者 | 单位 | E-mail | | 曹畅 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044
南京信息工程大学应用气象学院, 南京 210044 | ichangnj@sina.com | | 李旭辉 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044 | | | 张弥 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044
南京信息工程大学应用气象学院, 南京 210044 | | | 刘寿东 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044
南京信息工程大学应用气象学院, 南京 210044 | | | 肖薇 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044
南京信息工程大学应用气象学院, 南京 210044 | | | 肖启涛 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044
南京信息工程大学应用气象学院, 南京 210044 | | | 徐家平 | 南京信息工程大学Yale-NUIST大气环境中心, 南京 210044
南京信息工程大学应用气象学院, 南京 210044 | |
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| 中文摘要 |
| 湖表反照率是影响水-气界面能量平衡和水体内部光温环境的重要因子,受到太阳高度角、云量、风速和水质等环境因子的多重影响. 基于太湖中尺度涡度通量网4个涡度通量观测站点(梅梁湾、大浦口、避风港和小雷山)的辐射和风速资料,结合晴空指数和水质数据,分析上述因子对太湖湖表反照率的影响及太湖湖表反照率空间差异的原因. 主要结果为: 太阳高度角是控制湖表反照率日变化、季节变化的主要因子;太阳高度角低于35°且当晴空指数在0~0.1和0.4~0.6之间时湖表反照率出现高值. 反照率值呈现随风速、浊度和叶绿素a浓度升高而增大的趋势, 而风浪通过影响浅水湖泊浊度、叶绿素a浓度从而间接影响湖表反照率. 各站点湖表反照率关系为: 小雷山 >避风港 >大浦口 >梅梁湾,其中小雷山站位于草型和藻型湖区过渡区而梅梁湾站位于藻型湖区. 反照率与叶绿素a浓度水平之间的关系对蓝藻暴发及其严重程度并不敏感. 本研究为湖体反照率的参数化过程提供参考依据. |
| 英文摘要 |
| Lake surface albedo determines energy balance of water-atmospheric interface and water physical environment.Solar elevation angle, cloudiness, wind speed, water quality and other factors can affect lake surface albedo.Using solar radiation, wind speed, and water quality data (turbidity and chlorophyll-a concentration) which were observed in four eddy covariance sites (Meiliangwan, Dapukou, Bifenggang and Xiaoleishan i.e.MLW, DPK, BFG and XLS) in Lake Taihu and clearness index (kt), the influence of these factors on Lake Taihu surface albedo and the reasons that led to its spatial difference were investigated.The results showed that solar elevation angle played a leading role in the diurnal and seasonal change of lake surface albedo;lake surface albedo reached two peaks in 0< kt< 0.1 and 0.4< kt< 0.6 respectively, when solar elevation angle was below 35°.The surface albedo increased with the increasing wind speed, turbidity and chlorophyll-a concentration.However, wind could indirectly affect surface albedo through leading to the changes in sediment resuspension and chlorophyll-a distribution.The sequence of albedo in the four sites was XLS >BFG >DPK >MLW.XLS and BFG belonged to the higher albedo group, while DPK and MLW belonged to the lower albedo group.The different biological environments caused by aquatic macrophytes and algae resulting in the spatial variation of Lake Taihu surface albedo.The relationship between albedo and chlorophyll-a concentration was not a very sensitive factor for indicating the outbreak of algae.This study can provide theoretical reference for lake albedo parameterization. |
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