The glaciation of a cumulus cloud over New Mexico
The glaciation of a cumulus cloud over New Mexico
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新墨西哥州上空积云的冰川作用
DOI：
10.1002/qj.49712757503
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发表时间：
2001
影响因子：
8.9
通讯作者：
J. Latham
中科院分区：
文献类型：
--
作者：
V. Phillips;A. Blyth;P. Brown;T. Choularton;J. Latham
英国气象局云解析模式（CRM）和UMIST显式微物理模式（EMM）被用于分析1987年夏天在新墨西哥州上空形成的多热积云的机载研究数据。主要目标是对观测到的这片云的冰川作用发展建立定量的认识。
The Met Office Cloud Resolving Model (CRM) and the UMIST Explicit Microphysics Model (EMM) have been employed in the analysis of data from airborne studies of a multi‐thermal cumulus cloud which developed over New Mexico in the summer of 1987. The principal goal was to establish a quantitative understanding of the observed development of glaciation of this cloud.