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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Tropical intraseasonal oscillations in CFSv2 during Boreal summer and winter
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Tropical intraseasonal oscillations in CFSv2 during Boreal summer and winter

机译:夏季和冬季CFSv2中的热带季节性振荡

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摘要

The simulation of the tropical intraseasonal oscillations (ISOs) by a coupled model in the Indo-Pacific region is examined in this study. The retrospective forecasts by the Climate Forecast System version 2 (CFSv2) of National Centers of Environmental Prediction for the period 1982-2010 have been analysed and compared with observation. The leading Indian monsoon intraseasonal oscillation (MISO) during the boreal summer and the Madden-Julian Oscillation (MJO) during the boreal winter are extracted from daily precipitation anomalies in forecasts and observations by using a data-adaptive method. The model forecasts from May initial conditions simulates the observed spatial structure, magnitude and the northward and eastward propagation of MISO reasonably well. Similar performance is also evident in the simulation of the eastward propagating MJO in forecasts from November initial conditions. In the simulation of both the MISO and MJO by the model, the zonal wind at lower level shows appropriate observed relation with the precipitation and coupling with convection. The observed phase relations between precipitation and low-level relative vorticity and between precipitation and upper-level divergence in the zonal and meridional propagations are captured by the model. However, the variance of the ISOs differs from observation in certain regions, and the phase of the ISOs exhibits wide differences among the ensemble members of the forecast and with the observation. Comparison with the earlier model, CFS version 1, shows that the space-time structure and evolution of MISO and MJO are better simulated by CFSv2.
机译:在本研究中研究了印度太平洋地区耦合模型的热带渗透振荡(ISOS)的模拟。与观察相比,分析了1982-2010期国家环境预测中心的气候预测系统2(CFSv2)的回顾性预报。在北方夏季和北方冬季的狂欢夏季和MASO)领先的印度季风震荡(MISO)通过使用数据适应方法从预测和观察中的日常降水异常中提取出来的博尔冬季。从5月初始条件的模型预测模拟了MISO的观察到的空间结构,幅度和向东和向东传播。在11月初初始条件的预测中,在向东传播MJO的模拟中也显而易见的是。在模型的墨西和MJO的模拟中,较低水平的区域风显示了与对流的降水和耦合的适当观察到的关系。该模型捕获了沉淀和低水平相对涡度与沉淀和低水平相对涡度之间的相位关系以及沉淀和沉淀和上层分歧,由该模型捕获。然而,ISO的方差与某些区域的观察不同,并且ISO的阶段在预测的集合成员和观察中呈现宽差。与早期型号的比较CFS版本1,表明MISO和MJO的时空结构和演变更好地模拟CFSv2。

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