Showing 1 - 20 results of 246 for search '"Great Basin"', query time: 0.40s Refine Results
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    Changing fire regimes in the Great Basin USA by Eva K. Strand, Kori Blankenship, Corey Gucker, Mark Brunson, Eugénie MontBlanc

    Published 2025-02-01
    “…This study estimates how fire regimes have changed in the major Great Basin vegetation types over the past 60 years with comparisons to historical (pre‐1900) fire regimes. …”
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    WOOD CELLULAR DENDROCLIMATOLOGY: TESTING NEW PROXIES IN GREAT BASIN BRISTLECONE PINE by Emanuele Ziaco, Franco Biondi, Ingo Heinrich, Ingo Heinrich

    Published 2016-10-01
    “…Century-long (1870-2013) time series of anatomical parameters were developed for Great Basin bristlecone pine (Pinus longaeva D.K. Bailey) by capturing strongly contrasted microscopic images through a Confocal Laser Scanning Microscope. …”
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    Invertebrate community response to fire and rodent activity in the Mojave and Great Basin Deserts by Joshua D. Day, Jackson H. Birrell, Tyson J. Terry, Amy Clark, Phil Allen, Samuel B. St. Clair

    Published 2019-05-01
    “…The one exception was ant abundance, which was higher in rodent access plots than in rodent exclusion plots in June 2016, but only at the Great Basin site. Fire had little effect on the abundances of invertebrate groups at either desert site, with the exception of a negative effect on flying‐forager abundance at our Great Basin site. …”
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    Long‐term trajectories of fractional component change in the Northern Great Basin, USA by Matthew Rigge, Hua Shi, Collin Homer, Patrick Danielson, Brian Granneman

    Published 2019-06-01
    “…We report an automated method of mapping rangeland fractional component cover over a large portion of the Northern Great Basin, USA, from 1986 to 2016 using a dense Landsat imagery time series. …”
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    Fine-scale modeling of bristlecone pine treeline position in the Great Basin, USA by Jamis M Bruening, Tyler J Tran, Andrew G Bunn, Stuart B Weiss, Matthew W Salzer

    Published 2017-01-01
    “…Great Basin bristlecone pine ( Pinus longaeva ) and foxtail pine ( Pinus balfouriana ) are valuable paleoclimate resources due to their longevity and climatic sensitivity of their annually-resolved rings. …”
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    Archaeometric studies on rock art at four sites in the northeastern Great Basin of North America by Meinrat O. Andreae, Tracey W. Andreae

    Published 2022-01-01
    “…We derived age estimates for the rock art at four sites in the northern Great Basin region of North America based on DMn measurements on the petroglyphs and intact varnish. …”
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    A comparison of the effects of fire on rodent abundance and diversity in the Great Basin and Mojave Deserts. by Tiffanny R Sharp Bowman, Brock R McMillan, Samuel B St Clair

    Published 2017-01-01
    “…We experimentally tested the effects of fire on rodent communities of the Great Basin and Mojave Deserts. Fire decreased the abundance, richness, and diversity of rodents in the Great Basin after fire. …”
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    Sensitivity to weather drives Great Basin mesic resources and Greater Sage-Grouse productivity by Carl G. Lundblad, Christian A. Hagen, J. Patrick Donnelly, Skyler T. Vold, Ann M. Moser, Shawn P. Espinosa

    Published 2022-09-01
    “…We used over 70,000 greater sage-grouse (Centrocercus urophasianus) wings, derived from hunter harvest in three western states, to characterize spatiotemporal variation in sage-grouse productivity throughout the North American Great Basin during 1993 – 2020. We then tested the hypothesis that previously-identified associations between precipitation and sage-grouse productivity are mediated by the availability of mesic habitats, which provide the diet resources required by broods during typical late-summer seasonal drought. …”
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    A 350,000-year history of groundwater recharge in the southern Great Basin, USA by Tracie R. Jackson, Simon D. Steidle, Kathleen A. Wendt, Yuri Dublyansky, R. Lawrence Edwards, Christoph Spötl

    Published 2023-03-01
    “…Water-table changes in the southern Great Basin, USA, over the last 350,000 years are 3–4 times as sensitive to recharge changes during drier interglacial than wetter glacial conditions, according to modelling of groundwater flow model informed by paleo-water-level data.…”
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