- 积分
- 5456
- 贡献
-
- 精华
- 在线时间
- 小时
- 注册时间
- 2015-11-4
- 最后登录
- 1970-1-1
|
发表于 2021-4-30 13:57:32
|
显示全部楼层
以下是和吴佳老师邮件交流引用部分说明:
【引用说明】:
使用资料时,关于资料的说明和需要引用的文献为:
类似于Xu et al. (2009),数据集CN05.1使用距平逼近法(anomaly approach),由气候场和距平场分别插值后叠加得到(吴佳和高学杰, 2013),但使用了中国境内~2400个台站的观测资料。
As did by Xu et al. (2009), the CN05.1 dataset is constructed by the “anomaly approach” during the interpolation but with more station observations (~2400) in China (Wu and Gao, 2013). In the “anomaly approach”, a gridded climatology is first calculated, and then a gridded daily anomaly is added to the climatology to obtain the final dataset.
参考文献References:
1. Xu Y, Gao XJ, Shen Y, Xu CH, Shi Y, Giorgi F, 2009. A daily temperature dataset over China and its application in validating a RCM simulation. Advances in Atmospheric Sciences, 26(4), 763–772.
2.吴佳, 高学杰, 2013. 一套格点化的中国区域逐日观测资料及与其它资料的对比. 地球物理学报, 56(4): 1102-1111, doi: 10.6038g20130406 /// Wu J, Gao XJ, 2013, A gridded daily observation dataset over China region and comparison with the other datasets. Chinese Journal of Geophysics, 56(4): 1102-1111, doi: 10.6038g20130406(in Chinese with English abstract)
3. 风速引用:
1. Wu Jia, Gao Xuejie, Giorgi Filippo, Chen Deliang. Changes of effective temperature and cold/hot days in late decades over China based on a high resolution gridded observation dataset. Int. J. Climatol, 37(s1):788–800. DOI: 10.1002/joc.5038.
|
|