前言 海洋和大气相互制约,预报海表面温度变化所要考虑的因素之一是栈面上大气的温度变化.因此,准确预报出1 000hPa大气温度变化对提高海表面温度预报水平将有很大的帮助。 长期温度预报的方法有多种.如Adem的模式,它主要以热力学为基础;还有我国长期数值值预报小组和巢纪平等的模式.他们的预报结果都有一些很成功的预报个例,但仍需作大量的例子才能检验其方法的可倍度.最近陈英仪分析了10年冬季的500hPa高 Preface One of the factors to be considered in the ocean-atmosphere interaction and forecast of sea surface temperature changes is the temperature change of the atmosphere on the stack, so accurately predicting the atmospheric temperature change of 1 000 hPa will greatly help improve the prediction of the sea surface temperature . There are many ways to predict long-term temperature, such as Adem’s model, which is based on thermodynamics, long-term numerical forecasting team and Nest Mode of Equality, etc. Their forecast results include some very successful forecasts, But still need to make a large number of examples to test the scalability of its method.Recently Chen Yingyi 10 years of winter 500hPa high