Latent cooling and microphysics effects in deep convection

Fernandez-Gonzalez S.; Wang P. K.; Gascon E.; Valero F.; Sanchez J. L.

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Latent cooling and microphysics effects in deep convection

机译：深对流中的潜冷和微观物理效应

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Water phase changes within a storm are responsible for the enhancement of convection and therefore the elongation of its lifespan. Specifically, latent cooling absorbed during evaporation, melting and sublimation is considered the main cause of the intensification of downdrafts. In order to know more accurately the consequences of latent cooling caused by each of these processes (together with microphysical effects that they induce), four simulations were developed with the Wisconsin Dynamical and Microphysical Model (WISCDYMM): one with all the microphysical processes; other without sublimation; melting was suppressed in the third simulation; and evaporation was disabled in the fourth.

机译：暴风雨中的水相变化是对流增强的原因，因此延长了对流寿命。具体而言，在蒸发，熔化和升华过程中吸收的潜伏冷却被认为是下降气流加剧的主要原因。为了更准确地了解由这些过程中的每一个引起的潜在冷却的后果（以及它们引起的微物理效应），使用威斯康星动力学和微物理模型（WISCDYMM）开发了四个模拟：一个模拟涉及所有的微物理过程；其他无升华；在第三次模拟中熔化被抑制；第四，蒸发被禁用。

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来源
《Atmospheric research》 |2016年第11期|189-199|共11页
作者
Fernandez-Gonzalez S.; Wang P. K.; Gascon E.; Valero F.; Sanchez J. L.;
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作者单位

Univ Complutense Madrid, Fac CC Fis, Dpto Astrofis & CC Atmosfera, Ciudad Univ S-N, E-28040 Madrid, Spain;

Acad Sinica, Inst Earth Sci, Taipei, Taiwan;

Univ Leon, IMA, Atmospher Phys Grp, E-24071 Leon, Spain;

Univ Complutense Madrid, Fac CC Fis, Dpto Astrofis & CC Atmosfera, Ciudad Univ S-N, E-28040 Madrid, Spain;

Univ Leon, IMA, Atmospher Phys Grp, E-24071 Leon, Spain;

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正文语种 eng
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关键词
Cloud resolving model; Latent cooling; Microphysics;

机译：云解析模型潜冷微观物理学;

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Latent cooling and microphysics effects in deep convection

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