A Study on Future Projections of Precipitation Characteristics around Japan in Early Summer Combining GPM DPR Observation and CMIP5 Large-Scale Environments

Author:

Yokoyama Chie1,Takayabu Yukari N.1,Arakawa Osamu2,Ose Tomoaki3

Affiliation:

1. Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba, Japan

2. Japan Agency for Marine-Earth Science and Technology, Yokohama, Kanagawa, Japan

3. Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Ibaraki, Japan

Abstract

AbstractThis study estimates future changes in the early summer precipitation characteristics around Japan using changes in the large-scale environment, by combining Global Precipitation Measurement precipitation radar observations and phase 5 of the Coupled Models Intercomparison Project climate model large-scale projections. Analyzing satellite-based data, we first relate precipitation in three types of rain events (small, organized, and midlatitude), which are identified via their characteristics, to the large-scale environment. Two environmental fields are chosen to determine the large-scale conditions of the precipitation: the sea surface temperature and the midlevel large-scale vertical velocity. The former is related to the lower-tropospheric thermal instability, while the latter affects precipitation via moistening/drying of the midtroposphere. Consequently, favorable conditions differ between the three types in terms of these two environmental fields. Using these precipitation–environment relationships, we then reconstruct the precipitation distributions for each type with reference to the two environmental indices in climate models for the present and future climates. Future changes in the reconstructed precipitation are found to vary widely between the three types in association with the large-scale environment. In more than 90% of models, the region affected by organized-type precipitation will expand northward, leading to a substantial increase in this type of precipitation near Japan along the Sea of Japan, and in northern and eastern Japan on the Pacific side, where its present amount is relatively small. This result suggests an elevated risk of heavy rainfall in those regions because the maximum precipitation intensity is more intense in organized-type precipitation than in the other two types.

Funder

Japan Society for the Promotion of Science

The University of Tokyo

Japan Aerospace Exploration Agency

Environmental Restoration and Conservation Agency

Publisher

American Meteorological Society

Subject

Atmospheric Science

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