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Topography, relief, and TRMM‐derived rainfall variations along the Himalaya

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Bookhagen, Bodo, Burbank, Douglas W.·2006·Geophysical Research Letters

Abstract

Along the southern Himalayan topographic front, the Indian summer monsoon modulates erosive processes and rates. To investigate the influence of topography and relief on rainfall generation and resultant erosion, we processed satellite rainfall amounts for the last 8 years (1998–2005) from the Tropical Rainfall Measurement Mission (TRMM). Based upon a spatial resolution of ∼5 × 5 km for the Himalaya, we identify (1) the spatial distribution of rainfall and (2) the large‐scale relationships between topography, relief, and rainfall locations. Our results show two distinct rainfall maxima along strike in the Himalaya. The first, outer rainfall peak occurs along the southern margin of the Lesser Himalaya within a narrow band of mean elevation (0.9 ± 0.4 km) and mean relief (1.2 ± 0.2 km). The second, discontinuous, inner band typically occurs along the southern flank of the Greater Himalaya (elevation and relief: both 2.1 ± 0.3 km).

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Metadata

Authors
Bookhagen, B., & Burbank, D. W.
Venue
Geophysical Research Letters
Published
2006-04
Volume
33
Issue
8
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2010589603
Cited by
819
References
15
FWCI
9.15
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Topography, relief, and TRMM‐derived rainfall variations along the Himalaya. https://app.cochat.ai/papers/10.1029/2006gl026037
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Bookhagen, B., & Burbank, D. W. (2006). Topography, relief, and TRMM‐derived rainfall variations along the Himalaya. Geophysical Research Letters. https://doi.org/10.1029/2006gl026037

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