作者: Fan Ping , Zhexian Luo , Xiaofan Li
DOI: 10.1016/J.DYNATMOCE.2008.12.003
关键词:
摘要: Abstract The effects of ice microphysics on tropical atmospheric and oceanic variability are investigated with a two-dimensional coupled ocean-cloud resolving atmosphere model forced by the large-scale vertical velocity zonal wind derived from Tropical Ocean Global Atmosphere Coupled Response Experiment (TOGA COARE). experiment without is compared to control microphysics. Compared experiment, generates more humid colder suppressing stratiform clouds rainfall associated latent heating; produces saltier mixed layer larger saline forcing weaker rainfall. mixed-layer temperature insensitive