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美国纽约州立大学布法罗分校火山碎屑流和泥石流数学模型研究近况
引用本文:余斌.美国纽约州立大学布法罗分校火山碎屑流和泥石流数学模型研究近况[J].山地学报,2005,23(1):126-128.
作者姓名:余斌
作者单位:中国科学院水制部成都山地灾害与环境研究所,四川,成都,610041
基金项目:国家自然科学基金(40271003)资助项目~~
摘    要:美国国家科学基金会信息技术研究计划部批准了一项为期3a。金额为$1900000的山地物质流研究项目在UB执行。旨在运用技术手段提供尽可能准确的地质灾害(如火山和泥石流)信息给科学家、工程防治专家和生活在火山威胁阴影下的居民。SH模型和浅水方程组成了TITAN2D模型的基本方程。TITAN2D模拟了Colima,Casit,Little Tahoma Peak和San Bemardino Mountains等地区的火山和泥石流。

关 键 词:模型  火山碎屑流  泥石流
文章编号:1008-2786(2005)01-126-03
修稿时间:2004年12月2日

Research on the Numerical Model of Pyroclastic Flow and Debris Flow in the State University of New York at Buffalo, USA
YU Bin.Research on the Numerical Model of Pyroclastic Flow and Debris Flow in the State University of New York at Buffalo, USA[J].Journal of Mountain Research,2005,23(1):126-128.
Authors:YU Bin
Abstract:The highly ambitious, multidisciplinary work, which involves creation of simulations of active volcanoes, is being conducted under a three-year, $1.9 million grant from the National Science Foundation's Information Technology Research (ITR) Program on Feb. 21, 2002. The researchers will integrate simulation results, remote sensing data and geographic-information system data to organize and present the information to scientists, decision-makers and, ultimately, citizens. Some mountain area, such as Colima, Casita, Little Tahoma Peak and the San Bernardino Mountain were used to simulate geophysical flows by TITAN2D model.
Keywords:model  pyroclastic flow  debris flow
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