Zobrazeno 1 - 10
of 432
pro vyhledávání: '"Grant A. Meyer"'
Autor:
Ruchames, Louis
Publikováno v:
Negro History Bulletin, 1967 Mar 01. 30(3), 22-22.
Externí odkaz:
https://www.jstor.org/stable/24766772
Beaver activity can segment a stream corridor through dam building which locally affects channel slope and sediment transport. We have found, however, that long-term beaver presence within a river corridor has impacts beyond dam sites that affect sys
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::570477c6436651a6fc6d56028c007781
https://doi.org/10.5194/egusphere-egu2020-1210
https://doi.org/10.5194/egusphere-egu2020-1210
Autor:
Rebekah Levine, Grant A. Meyer
Publikováno v:
Scientific Reports, Vol 9, Iss 1, Pp 1-12 (2019)
Scientific Reports
Scientific Reports
Given the direct effects of their dams on hydrology, sediment storage, and vegetation, beaver are widely acknowledged as ecosystem engineers. Here we explore the effects of beaver activity on channel processes and riparian plant recruitment beyond th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e1151a2e3e3272d51f04e3e15e36774
https://doi.org/10.1038/s41598-019-44381-2
https://doi.org/10.1038/s41598-019-44381-2
Autor:
Rebekah Levine, Grant A. Meyer
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::569d35a8bd830e242f27c149801c8e65
https://doi.org/10.1130/abs/2019am-341109
https://doi.org/10.1130/abs/2019am-341109
Autor:
Lyman P. Persico, Grant A. Meyer
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95df4d02c672f4900441ee88e27771cb
https://doi.org/10.1130/abs/2019am-341378
https://doi.org/10.1130/abs/2019am-341378
Autor:
Grant A. Meyer, Erin P. Fitch
Publikováno v:
Quaternary Research. 85:75-86
In the Jemez Mountains, tree-ring data indicate that low-severity fires characterized the 400 yr before Euro-American settlement, and that subsequent fire suppression promoted denser forests, recent severe fires, and erosion. Over longer timescales,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::361c3a423c6f60cf970646faa0a4c337
https://doi.org/10.1016/j.yqres.2015.11.008
https://doi.org/10.1016/j.yqres.2015.11.008
Publikováno v:
The Holocene. 25:857-871
The Middle Fork Salmon River watershed spans high-elevation mixed-conifer forests to lower-elevation shrub-steppe. In recent decades, runoff from severely burned hillslopes has generated large debris flows in steep tributary drainages. These flows in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f94e2571297d4d2c2ddb5363575af1a3
https://doi.org/10.1177/0959683615571423
https://doi.org/10.1177/0959683615571423
Autor:
Joseph R. McAuliffe, Grant A. Meyer, Tim Wawrzyniec, Leah M. Roberts, Louis A. Scuderi, Matthew P. King, Leslie D. McFadden
Publikováno v:
Global and Planetary Change. 122:1-13
Pinyon–juniper woodlands of the western United States frequently exist within topographically complex landscapes where varied slope aspect yields substantial, local microclimate variation. Vegetation composition and cover typically change markedly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af36ccf99413525c91255e22dbcf8824
https://doi.org/10.1016/j.gloplacha.2014.07.008
https://doi.org/10.1016/j.gloplacha.2014.07.008
Autor:
Benjamin J. Swanson, Grant A. Meyer
Publikováno v:
Earth Surface Processes and Landforms. 39:1927-1943
Numerous morphological changes can occur where two channels of distinct sediment and flow regimes meet, including abrupt shifts in channel slope, cross-sectional area, planform style, and bed sediment size along the receiving channel. Along the Rio C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee797272d4c7df7cf9d1d49871d2d6ad
https://doi.org/10.1002/esp.3586
https://doi.org/10.1002/esp.3586