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Sensitivity studies of the RegCM3 simulation of summer precipitation, temperature and local wind field in the Caribbean Region

机译:RegCM3模拟加勒比地区夏季降水,温度和局部风场的敏感性研究

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We present a preliminary evaluation of the performance of three different cumulus parameterization schemes in the ICTP Regional Climate Model RegCM3 for two overlapping domains (termed "big" and "small") and horizontal resolutions (50 and 25 km) in the Caribbean area during the summer (July-August-September). The cumulus param-eterizations were the Grell scheme with two closure assumptions (Arakawa-Schubert and Fritsch-Chappell) and the Anthes-Kuo scheme. An additional sensitivity test was performed by comparing two different flux parameterization schemes over the ocean (Zeng and BATS). There is a systematic underestimation of air temperature and precipitation when compared with analyzed data over the big domain area. Greater (~2℃) and smaller (~0.9℃) negative temperature biases are obtained in Grell-FC and Kuo convective scheme, respectively, and intermediate values are obtained in Grell-AS. The small domain simulation produces results substantially different, both for air temperature and precipitation. Temperature estimations are better for the small domain, while the precipitation estimations are better for the big domain. An additional experiment showed that by using BATS to calculate the ocean fluxes in the big domain instead of the Zeng scheme, precipitation increases by 25% and the share of convective precipitation rose from 18% to 45% of the total, which implies a better simulation of precipitation. These changes were attributed to an increase of near surface latent heating when using BATS over the ocean. The use of BATS also reduces the cold bias by about 0.3-0.4℃, associated with an increase of minimum temperature. The behavior of the precipitation diurnal cycle and its relation with sea breeze was investigated in the small domain experiments. Results showed that the Grell-Arakawa-Schubert closure describes better this circulation as compared with Grell-Fritsch-Chappell closure.
机译:我们对ICTP区域气候模型RegCM3中三个重叠域(称为“大”和“小”)和水平分辨率(50和25 km)在加勒比海地区的三种不同积云参数化方案的性能进行了初步评估。夏天(7月-8月-9月)。累积参数化是具有两个封闭假设(Arakawa-Schubert和Fritsch-Chappell)的Grell方案和Anthes-Kuo方案。通过比较两种不同的海洋通量参数化方案(Zeng和BATS),进行了附加的灵敏度测试。与大范围区域内的分析数据相比,系统地低估了气温和降水。在Grell-FC和Kuo对流方案中分别获得较大的(〜2℃)和较小的(〜0.9℃)负温度偏差,在Grell-AS中获得中间值。小域模拟产生的结果在气温和降水方面都大不相同。对于小范围,温度估计更好,而对于大范围,降水估计更好。另一个实验表明,通过使用BATS而不是Zeng方案来计算大域中的海洋通量,降水量增加了25%,对流降水量的比例从总量的18%上升到45%,这意味着更好的模拟降水。这些变化归因于在海洋上使用BATS时近地表潜热的增加。使用BATS还可以将冷偏差降低约0.3-0.4℃,从而降低最低温度。在小范围实验中研究了降水日循环的行为及其与海风的关系。结果表明,与Grell-Fritsch-Chappell封闭相比,Grell-Arakawa-Schubert封闭更好地描述了这种循环。

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