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contributor authorKanamori, Hironari
contributor authorKumagai, Tomo’omi
contributor authorFujinami, Hatsuki
contributor authorHiyama, Tetsuya
contributor authorYasunari, Tetsuzo
date accessioned2019-09-19T10:02:11Z
date available2019-09-19T10:02:11Z
date copyright8/9/2018 12:00:00 AM
date issued2018
identifier otherjhm-d-18-0052.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4260831
description abstractAbstractThis study investigated atmospheric water cycles over several time scales to understand the maintenance processes that control heavy precipitation over the islands of the Maritime Continent. Large island regions can be divided into land, coastal, and ocean areas based on the characteristics of both the hydrologic cycle and the diurnal variation in precipitation. Within the Maritime Continent, the major islands of Borneo and New Guinea exhibit different hydrologic cycles. Large-scale circulation variations, such as the seasonal cycle and the Madden?Julian oscillation, have a lesser effect on the hydrologic cycle over Borneo than over New Guinea because the effects depend on their shapes and locations. The impact of diurnal variations on both regional-scale circulation and water exchange between land and coastal regions is pronounced over both islands. The recycling ratio of precipitation, which can be related to stronger diurnal variation in the atmospheric water cycle that results from enhanced evapotranspiration over tropical rain forests, is higher over Borneo than over New Guinea.
publisherAmerican Meteorological Society
titleEffects of Long- and Short-Term Atmospheric Water Cycles on the Water Balance over the Maritime Continent
typeJournal Paper
journal volume19
journal issue9
journal titleJournal of Hydrometeorology
identifier doi10.1175/JHM-D-18-0052.1
journal fristpage1413
journal lastpage1427
treeJournal of Hydrometeorology:;2018:;volume 019:;issue 009
contenttypeFulltext


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