Effects of post-fire logging on forest surface air temperatures in the Siskiyou Mountains, Oregon, USA
Author(s) -
Joseph B. Fontaine,
Daniel C. Donato,
John L. Campbell,
Jonathan G. Martin,
B. E. Law
Publication year - 2010
Publication title -
forestry an international journal of forest research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.747
H-Index - 63
eISSN - 1464-3626
pISSN - 0015-752X
DOI - 10.1093/forestry/cpq030
Subject(s) - salvage logging , environmental science , logging , snag , vegetation (pathology) , pine forest , disturbance (geology) , forestry , growing season , air temperature , climate change , hydrology (agriculture) , atmospheric sciences , ecology , geography , geology , biology , geotechnical engineering , pathology , habitat , medicine , paleontology
Summary Following stand-replacing wildfire, post-fire (salvage) logging of fire-killed trees is a widely implemented management practice in many forest types. A common hypothesis is that removal of fire-killed trees increases surface temperatures due to loss of shade and increased solar radiation, thereby influencing vegetation establishment and possibly stand development. Six years after a wildfire in a Mediterranean-climate mixed-conifer forest in southwest Oregon, USA, we measured the effects of post-fire logging (>90 per cent dead tree (snag) removal) on growing season surface air temperatures. Compared with unlogged severely burned forest, post-fire logging did not lead to increased maximum daily surface air temperature. However, dead tree removal was associated with lower nightly minimum temperatures (~1°C) and earlier daytime heating, leading to a 1–2°C difference during the warming portion of the day. Effects varied predictably by aspect. The patterns reported here represent a similar but muted pattern as previously reported for microclimatic changes following clear-cutting of green trees. Effects of microsites such as tree bases on fine-scale temperature regimes require further investigation.
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