Assimilation and High Resolution Forecasts of Surface and Near Surface Conditions for the 2010 Vancouver Winter Olympic and Paralympic Games

被引:11
作者
Bernier, Natacha B. [1 ]
Belair, Stephane [1 ]
Bilodeau, Bernard [1 ]
Tong, Linying [2 ]
机构
[1] Environm Canada, Meteorol Res Div, Dorval, PQ H9P 1J3, Canada
[2] Environm Canada, Canadian Meteorol Ctr, Dorval, PQ, Canada
基金
英国科研创新办公室;
关键词
Point forecast; assimilation; land surface forecast system; NUMERICAL WEATHER PREDICTION; OPERATIONAL IMPLEMENTATION; MODEL; SNOW; SYSTEM; PARAMETERIZATION; VALIDATION; CANADA; SCHEME;
D O I
10.1007/s00024-012-0542-0
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A dynamical model was experimentally implemented to provide high resolution forecasts at points of interests in the 2010 Vancouver Olympics and Paralympics Region. In a first experiment, GEM-Surf, the near surface and land surface modeling system, is driven by operational atmospheric forecasts and used to refine the surface forecasts according to local surface conditions such as elevation and vegetation type. In this simple form, temperature and snow depth forecasts are improved mainly as a result of the better representation of real elevation. In a second experiment, screen level observations and operational atmospheric forecasts are blended to drive a continuous cycle of near surface and land surface hindcasts. Hindcasts of the previous day conditions are then regarded as today's optimized initial conditions. Hence, in this experiment, given observations are available, observation driven hindcasts continuously ensure that daily forecasts are issued from improved initial conditions. GEM-Surf forecasts obtained from improved short-range hindcasts produced using these better conditions result in improved snow depth forecasts. In a third experiment, assimilation of snow depth data is applied to further optimize GEM-Surf's initial conditions, in addition to the use of blended observations and forecasts for forcing. Results show that snow depth and summer temperature forecasts are further improved by the addition of snow depth data assimilation.
引用
收藏
页码:243 / 256
页数:14
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