作业帮求英语作文,要初一的水平
来源：学生作业帮 编辑：作业帮 分类：英语作业 时间：2024/05/12 04:16:21
求英语作文,要初一的水平
描述自己,有关自己的爱好,特长,介绍自己家庭情况,用一般现在时,介绍自己最好的朋友,用第三人称单数
描述自己,有关自己的爱好,特长,介绍自己家庭情况,用一般现在时,介绍自己最好的朋友,用第三人称单数
An example of hindcasting would be entering climate forcings (events that force change) into a climate model. If the hindcast accurately showed weather events that are known to have occurred, the model would be considered successful.
In oceanography and meteorology, hindcasting usually refers to a numerical model integration of a historical period where no observations have been assimilated. This distinguishes a hindcast run from a reanalysis. Oceanographic observations of salinity and temperature as well as observations of surface wave parameters such as the significant wave height are much scarcer than meteorological observations, making hindcasting more common in oceanography than in meteorology. Also, since surface waves represent a forced system where the wind is the only generating force, wave hindcasting is often considered adequate for generating a reasonable representation of the wave climate with litte need for a full reanalysis.
The ECMWF re-analysis is an example of a combined atmospheric reanalysis coupled with a wave model integration where no wave parameters were assimilated, making the wave part a hindcast run.
In oceanography and meteorology, hindcasting usually refers to a numerical model integration of a historical period where no observations have been assimilated. This distinguishes a hindcast run from a reanalysis. Oceanographic observations of salinity and temperature as well as observations of surface wave parameters such as the significant wave height are much scarcer than meteorological observations, making hindcasting more common in oceanography than in meteorology. Also, since surface waves represent a forced system where the wind is the only generating force, wave hindcasting is often considered adequate for generating a reasonable representation of the wave climate with litte need for a full reanalysis.
The ECMWF re-analysis is an example of a combined atmospheric reanalysis coupled with a wave model integration where no wave parameters were assimilated, making the wave part a hindcast run.