一般的非绝热加热数据,需要通过WRF输出,原因如下两点:
Answer:
RTHCUTEN (from cumulus), RTHRATEN (from radiation), RTHBLTEN (from PBL parameterization), RTHNDGDTEN (if nudging is applied), and H_DIABATIC总的非绝热加热率这里简单表达为:
Q = Q m i c r o p h y s i c s + Q b o u n d a r y l a y e r + Q r a d i a t i o n + Q c u m u l u s Q=Q_{\mathrm{microphysics}}+Q_{\mathrm{boundary _layer}}+Q_{\mathrm{radiation}}+Q_{\mathrm{cumulus}} Q=Qmicrophysics+Qboundarylayer+Qradiation+Qcumulus
分别表示由云微物理过程、边界层通量交换、辐射过程和积云对流过程产生的非绝热加热过程。
对于多层嵌套网格,可能去掉积云对流参数化过程的那一项,只使用前三项
主要有两个方式,在之前的博文中有过详细介绍,这里不展开叙述了。
[1] Luo, H., & Yanai, M. (1984). The Large-Scale Circulation and Heat Sources over the Tibetan Plateau and Surrounding Areas during the Early Summer of 1979. Part II: Heat and Moisture Budgets, Monthly Weather Review, 112(5), 966-989.
[2] Hoskins, B. J., McIntyre, M., & Robertson, A. W. (1985). On the use and significance of isentropic potential vorticity maps. Quarterly Journal of the Royal Meteorological Society, 111(470), 877–946.https://forum.mmm.ucar.edu/threads/adding-diabatic-heating-rates-to-wrf-arw-real-outputs.5423/
https://forum.mmm.ucar.edu/threads/latent-heating-from-cumulus-parameterization.8797/
https://forum.mmm.ucar.edu/threads/microphysics-heating-tendency-and-relationship-with-cumulus-scheme.9738/#p19094