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Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

From: Outcomes and challenges of global high-resolution non-hydrostatic atmospheric simulations using the K computer

Fig. 6

Horizontal distribution of OLR comparing Asian monsoon between simulations and observation. a National Oceanic and Atmospheric Administration (NOAA) OLR and b OLR of the NICAM AMIP-type simulation defined by the difference between the annual maximum and minimum OLR in the pentad mean climatology (1979–2008). The northern Australia-Indonesia monsoon (NAIM), Southeast Asian monsoon (SEAM), and western North Pacific monsoon (WNPM) are identified after Murakami and Matsumoto (1994)

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