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Image JPEG image Imitator salamander, melanistic phase_squamatologist
Imitator salamander
Located in Research / / Assessing Vulnerability of Species and Habitats to Large-scale Impacts / Species and Habitat Vulnerability Assessment Photo Gallery
File PDF document Imlay 1972.pdf
Located in Resources / TRB Library / HUE-JOH
File PDF document Imlay 1973 Potassium.pdf
Located in Resources / TRB Library / HUE-JOH
File PDF document Imlay 1973.pdf
Located in Resources / TRB Library / HUE-JOH
File PDF document Imlay 1977.pdf
Located in Resources / TRB Library / HUE-JOH
File PDF document Imlay Environmental Stimulus.pdf
Located in Resources / TRB Library / HUE-JOH
File PDF document Imlay Vita Publications.pdf
Located in Resources / TRB Library / HUE-JOH
File PDF document Impact of a Century of Climate Change on Small-Mammal Communities in Yosemite National Park, USA
We provide a century-scale view of small-mammal responses to global warming, without confounding effects of land-use change, by repeating Grinnell’s early–20th century survey across a 3000-meter-elevation gradient that spans Yosemite National Park, California, USA. Using occupancy modeling to control for variation in detectability, we show substantial (~500 meters on average) upward changes in elevational limits for half of 28 species monitored, consistent with the observed ~3°C increase in minimum temperatures. Formerly low-elevation species expanded their ranges and high-elevation species contracted theirs, leading to changed community composition at mid- and high elevations. Elevational replacement among congeners changed because species’ responses were idiosyncratic. Though some high-elevation species are threatened, protection of elevation gradients allows other species to respond via migration
Located in Resources / Climate Science Documents
File PDF document Impact of deforestation in the Amazon basin on cloud climatology
Shallow clouds are prone to appear over deforested surfaces whereas deep clouds, much less frequent than shallow clouds, favor forested surfaces. Simultaneous atmospheric soundings at forest and pasture sites during the Rondonian Boundary Layer Experiment (RBLE-3) elucidate the physical mechanisms responsible for the observed correlation between clouds and land cover. We demonstrate that the atmospheric boundary layer over the forested areas is more unstable and characterized by larger values of the convective available potential energy (CAPE) due to greater humidity than that which is found over the deforested area. The shallow convection over the deforested areas is relatively more active than the deep convection over the forested areas. This greater activity results from a stronger lifting mechanism caused by mesoscale circulations driven by deforestation-induced heterogeneities in land cover. climate 􏰅 land-cover heterogeneity 􏰅 mesoscale circulations
Located in Resources / Climate Science Documents
File PDF document Impact of disturbed desert soils on duration of mountain snow cover
Snow cover duration in a seasonally snow covered mountain range (San Juan Mountains, USA) was found to be shortened by 18 to 35 days during ablation through surface shortwave radiative forcing by deposition of disturbed desert dust. Frequency of dust deposition and radiative forcing doubled when the Colorado Plateau, the dust source region, experienced intense drought (8 events and 39–59 Watts per square meter in 2006) versus a year with near normal precipitation (4 events and 17–34 Watts per square meter in 2005). It is likely that the current duration of snow cover and surface radiation budget represent a dramatic change from those before the widespread soil disturbance of the western US in the late 1800s that resulted in enhanced dust emission. Moreover, the projected increases in drought intensity and frequency and associated increases in dust emission from the desert southwest US may further reduce snow cover duration
Located in Resources / Climate Science Documents