P
Philip W. Mote
Researcher at Oregon State University
Publications - 104
Citations - 13490
Philip W. Mote is an academic researcher from Oregon State University. The author has contributed to research in topics: Climate change & Climate model. The author has an hindex of 44, co-authored 103 publications receiving 12213 citations. Previous affiliations of Philip W. Mote include Pennsylvania State University & Joint Institute for the Study of the Atmosphere and Ocean.
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Journal ArticleDOI
Declining mountain snowpack in western north america
TL;DR: In this article, the authors examined manual and telemetered measurements of spring snowpack, corroborated by a physically based hydrologic model, for climate-driven fluctuations and trends during the period of 1916-2002.
Observations: Changes in Snow, Ice and Frozen Ground
Peter Lemke,Jian Ren,Richard B. Alley,Ian Allison,Jorge F. Carrasco,Gregory M. Flato,Yoshiyuki Fujii,Georg Kaser,Philip W. Mote,Robert H. Thomas,Tingjun Zhang +10 more
TL;DR: Contributing Authors: J.H. Box, D.O. Robinson, Ian Joughin, S. Smith, and D.W. Walsh.
Journal ArticleDOI
Tropical tropopause layer
TL;DR: The Tropical Tropopause Layer (TTL) as discussed by the authors is a 3D model of the troposphere, and it has been shown that the transition from troposphere to stratosphere occurs in a layer, rather than at a sharp "tropopause".
Journal ArticleDOI
An atmospheric tape recorder: The imprint of tropical tropopause temperatures on stratospheric water vapor
Philip W. Mote,Karen H. Rosenlof,Michael E. McIntyre,Ewan S. Carr,John C. Gille,James R. Holton,Jonathan S. Kinnersley,Hugh C. Pumphrey,James M. Russell,Joe W. Waters +9 more
TL;DR: In this paper, the authors describe observations of tropical stratospheric water vapor q that show clear evidence of large-scale upward advection of the signal from annual fluctuations in the effective "entry mixing ratio" qE of air entering the tropical stratosphere.
Journal ArticleDOI
Climatic Change, Wildfire, and Conservation
TL;DR: In this article, the authors show that climate variability is a dominant factor affecting large wildfires in the western United States, an observation supported by palaeoecological data on charcoal in lake sediments and reconstructions from fire-scarred trees.