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International Journal of Earth & Environmental Sciences Volume 1 (2016), Article ID 1:IJEES-104, 7 pages
https://doi.org/10.15344/2456-351X/2016/104
Research Article
Spatial Characteristics of Rainfall at Sparsely Distributed Station Network over the High-Latitude Mountainous Regions in Eastern Siberia

Konosuke Sugiura1,2*, Shuhei Takahashi3, Takao Kameda4, Hiroyuki Enomoto5, Yuliy Kononov6 and Maria Ananicheva6

1University of Toyama, 3190 Gofuku, Toyama 930-8555, Japan
2Japan Agency for Marine-Earth Science and Technology, 3173-25, Showamachi, Kanazawa-ku, Yokohama 236-0001, Japan
3Okhotsk Sea Ice Museum of Hokkaido, 11-6, Motomombetsu, Mombetsu, Hokkaido 094-0023, Japan
4Kitami Institute of Technology, 165, Koencho, Kitami 090-8507, Japan
5Inter-university Research Institute Corporation Research Organization of Information and Systems, National Institute of Polar Research, 10-3, Midoricho, Tachikawa 190-8518, Japan
6Institute of Geography, Russian Academy of Science, Staromonetniy pereulok 29, Moscow 119017, Russia
Dr. Konosuke Sugiura, University of Toyama, 3190 Gofuku, Toyama 930-8555, Japan, Japan; E-mail: sugiura@sci.u-toyama.ac.jp
30 January 2016; 09 April 2016; 11 April 2016
Sugiura K, Takahashi S, Kameda T, Enomoto H, Kononov Y, et al. (2016) Spatial Characteristics of Rainfall at Sparsely Distributed Station Network over the High-Latitude Mountainous Regions in Eastern Siberia. Int J Earth Environ Sci 1: 104. doi: https://doi.org/10.15344/2456-351X/2016/104
This research was partially supported by a Ministry of Education, Science, Sports and Culture Grant-in-Aid for Scientific Research (B), 16403006, 2004-2007, Glaciological observations in Eastern Siberia as an activity of IPY project entitled "Glaciological research in Suntar Khayata Range, East Siberia, Russia, for International Polar Year" (ID No. 393).

Abstract

To describe the spatial characteristics of rainfall at sparsely distributed measurement network over the high-latitude mountainous regions in eastern Siberia through ground-based observation, rainfall observations were performed using non-recording standard rain gauges. Such standard rain gauges have been used over the years to measure annual rainfall at six sites from the Suntar Khayata Range to Oymyakon and 12 sites along the Kolyma Highway from Magadan to Agayakan. Relational expressions of rainfall were obtained and observation data from these gauges clearly showed that the corrected rainfall in these areas depends on altitude, that the rainfall increased slightly with an increase in altitude, and that the increased ratio of rainfall due to altitude decreased with an increase in the distance from the nearby coast.