The set-up and evaluation of fine-scale data assimilation for the urban climate of Amsterdam

被引:6
|
作者
Koopmans, Sytse [1 ,5 ]
van Haren, Ronald [2 ]
Theeuwes, Natalie [1 ,3 ]
Ronda, Reinder [1 ]
Uijlenhoet, Remko [4 ]
Holtslag, Albert A. M. [1 ]
Steeneveld, Gert-Jan [1 ,5 ]
机构
[1] Wageningen Univ, Meteorol & Air Qual Sect, Wageningen, Netherlands
[2] Netherlands Esci Ctr, Amsterdam, Netherlands
[3] Royal Netherlands Meteorol Inst KNMI, De Bilt, Netherlands
[4] Delft Univ Technol, Hydrol Sect, Delft, Netherlands
[5] Wageningen Univ, Meteorol & Air Qual Sect, POB 47, NL-6700 AA Wageningen, Netherlands
基金
英国工程与自然科学研究理事会;
关键词
CITIZEN WEATHER STATIONS; CANOPY MODEL; ERA-INTERIM; HEAT-ISLAND; IMPACT; TEMPERATURE; ENERGY; VERIFICATION; VARIABILITY; PREDICTION;
D O I
10.1002/qj.4401
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Ongoing urbanization highlights the need for a better understanding and high resolution modelling of the urban climate. In this study, we combine rural observations by WMO surface stations, weather radar data and urban crowd-sourced observations with very fine-scale modelling efforts for Amsterdam, The Netherlands. As a model, we use the Weather Research and Forecasting (WRF) mesoscale model with 3D variational data assimilation at a 100-m resolution in the innermost model domain. In order to enable the assimilation of observations within the urban canopy, we develop a scheme to reduce urban temperature biases by adjusting urban fabric temperatures. The scheme is tested against independent urban observations for the summer month of July 2014 and specifically for a hot period and an extreme precipitation event. We find data assimilation reduces biases in temperature and wind speed. Within the city, the most significant improvement is the reduction of negative temperature biases during clear nights, which implies a better prediction of the Urban Heat Island (UHI). Concerning precipitation, the fractional skill score improves incrementally when additional observations are assimilated, and the largest impact is seen from the assimilation of weather radar observations.
引用
收藏
页码:171 / 191
页数:21
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