scholarly journals Bidirectional recovery patterns of Mojave Desert vegetation in an aqueduct pipeline corridor after 36 years: I. Perennial shrubs and grasses

2016 ◽  
Vol 124 ◽  
pp. 413-425 ◽  
Author(s):  
Kristin H. Berry ◽  
James F. Weigand ◽  
Timothy A. Gowan ◽  
Jeremy S. Mack
1979 ◽  
Vol 3 (6) ◽  
pp. 517-529 ◽  
Author(s):  
Robert H. Webb ◽  
Steven S. Stielstra

2015 ◽  
Vol 122 ◽  
pp. 141-153 ◽  
Author(s):  
Kristin H. Berry ◽  
Jeremy S. Mack ◽  
James F. Weigand ◽  
Timothy A. Gowan ◽  
Denise LaBerteaux

2013 ◽  
Vol 66 (2) ◽  
pp. 311-322 ◽  
Author(s):  
Ross J. Guida ◽  
Scott R. Abella ◽  
William J. Smith ◽  
Haroon Stephen ◽  
Chris L. Roberts

2020 ◽  
Vol 11 (4) ◽  
pp. 79-100
Author(s):  
Ross J. Guida ◽  
Scott R. Abella

While it is often the assumption in environmental modeling that finer-resolution modeling is preferred, especially if computation times are not prohibitive, few studies have assessed how climate grid resolution influences the Maxent-predicted habitat of desert vegetation species. Further, drought events can occur over longer or shorter terms with drought length potentially influencing species' habitat distributions. This study uses four higher-elevation Mojave Desert plant species experiencing known habitat contractions corresponding with climatic changes to assess how sensitive Maxent species distribution models are to using 5- and 10-year averaged climate data, as well as 800-m and 4-km resampled gridded climate data. Results show there are spatial differences in models despite relatively consistent clustering of three of the species' recorded field locations, whereas predicting habitat for the more broadly ranging species results in less certainty across all models. Overall, models were more sensitive to the spatial resolution of the climate data than to the climate time step used. When considering geographic areas with high relief, such as the Newberry Mountains in southern Nevada constituting the study area, the spatial resolution of climate data has a major influence on modeled habitat. As more fine-resolution climate data become available, researchers may need to establish more plots for field collection to assess specific microclimatic effects on vegetation.


1983 ◽  
Vol 19 (2) ◽  
pp. 256-264 ◽  
Author(s):  
W. Geoffrey Spaulding

AbstractUntil recently, the oldest-known packrat (Neotoma spp.) midden records of desert scrub vegetation were less than 10,500 yr old and were restricted to altitudes below 300 m in the northern Sonoran Desert. Recent discovery of macrofossil assemblages in the Mojave Desert extends the record of desert vegetation back to 14,800 yr ago and to altitudes as high as 910 m. Although xerophytic conifer woodland was widespread in current desert habitats during the Late Wisconsin and early Holocene, the development of extensive desert vegetation was not delayed until the beginning of the middle Holocene. A regional vegetation mosaic of desert scrub and woodland existed at altitudes below 1000 m in the Mojave Desert during the last part of the Late Wisconsin.


2008 ◽  
Author(s):  
David M. Miller ◽  
Debra Hughson ◽  
Kevin M. Schmidt
Keyword(s):  

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