Present, future, and novel bioclimates of the San Francisco, California region

Bioclimates are syntheses of climatic variables into biologically relevant categories that facilitate comparative studies of biotic responses to climate conditions. Isobioclimates, unique combinations of bioclimatic indices (continentality, ombrotype, and thermotype), were constructed for northern C...

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Published in:PloS one 2013-03, Vol.8 (3), p.e58450
Main Authors: Torregrosa, Alicia, Taylor, Maxwell D, Flint, Lorraine E, Flint, Alan L
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title Present, future, and novel bioclimates of the San Francisco, California region
format Article
creator Torregrosa, Alicia
Taylor, Maxwell D
Flint, Lorraine E
Flint, Alan L
subjects Bioclimatic indexes
Bioclimatology
Biogeography
Biology
Biometeorology
Climate
Climate change
Climate Change - classification
Climate Change - statistics & numerical data
Climate models
Climatic conditions
Climatology
Comparative analysis
Comparative studies
Computational fluid dynamics
Computer Science
Conservation of Natural Resources
Continentality
Digital mapping
Dispersal
Drought
Earth Sciences
Ecosystem
Emission analysis
Flowers & plants
Fluid dynamics
Future climates
Geography
Geology
Geophysical fluids
Geophysics
Hydrodynamics
Models, Theoretical
Ordination
Patches (structures)
Photosynthesis
Phylogeography
Plants
Precipitation
San Francisco
Science
Social and Behavioral Sciences
Spatial discrimination
Spatial resolution
Temperature
Trees
Vegetation
Vegetation distribution
ispartof PloS one, 2013-03, Vol.8 (3), p.e58450
description Bioclimates are syntheses of climatic variables into biologically relevant categories that facilitate comparative studies of biotic responses to climate conditions. Isobioclimates, unique combinations of bioclimatic indices (continentality, ombrotype, and thermotype), were constructed for northern California coastal ranges based on the Rivas-Martinez worldwide bioclimatic classification system for the end of the 20(th) century climatology (1971-2000) and end of the 21(st) century climatology (2070-2099) using two models, Geophysical Fluid Dynamics Laboratory (GFDL) model and the Parallel Climate Model (PCM), under the medium-high A2 emission scenario. The digitally mapped results were used to 1) assess the relative redistribution of isobioclimates and their magnitude of change, 2) quantify the loss of isobioclimates into the future, 3) identify and locate novel isobioclimates projected to appear, and 4) explore compositional change in vegetation types among analog isobioclimate patches. This study used downscaled climate variables to map the isobioclimates at a fine spatial resolution -270 m grid cells. Common to both models of future climate was a large change in thermotype. Changes in ombrotype differed among the two models. The end of 20(th) century climatology has 83 isobioclimates covering the 63,000 km(2) study area. In both future projections 51 of those isobioclimates disappear over 40,000 km(2). The ordination of vegetation-bioclimate relationships shows very strong correlation of Rivas-Martinez indices with vegetation distribution and composition. Comparisons of vegetation composition among analog patches suggest that vegetation change will be a local rearrangement of species already in place rather than one requiring long distance dispersal. The digitally mapped results facilitate comparison with other Mediterranean regions. Major remaining challenges include predicting vegetation composition of novel isobioclimates and developing metrics to compare differences in climate space.
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Isobioclimates, unique combinations of bioclimatic indices (continentality, ombrotype, and thermotype), were constructed for northern California coastal ranges based on the Rivas-Martinez worldwide bioclimatic classification system for the end of the 20(th) century climatology (1971-2000) and end of the 21(st) century climatology (2070-2099) using two models, Geophysical Fluid Dynamics Laboratory (GFDL) model and the Parallel Climate Model (PCM), under the medium-high A2 emission scenario. The digitally mapped results were used to 1) assess the relative redistribution of isobioclimates and their magnitude of change, 2) quantify the loss of isobioclimates into the future, 3) identify and locate novel isobioclimates projected to appear, and 4) explore compositional change in vegetation types among analog isobioclimate patches. This study used downscaled climate variables to map the isobioclimates at a fine spatial resolution -270 m grid cells. 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Performed the experiments: AT MT LF AF. Analyzed the data: AT MT LF AF. Contributed reagents/materials/analysis tools: AT LF AF. Wrote the paper: AT MT.</notes><abstract>Bioclimates are syntheses of climatic variables into biologically relevant categories that facilitate comparative studies of biotic responses to climate conditions. Isobioclimates, unique combinations of bioclimatic indices (continentality, ombrotype, and thermotype), were constructed for northern California coastal ranges based on the Rivas-Martinez worldwide bioclimatic classification system for the end of the 20(th) century climatology (1971-2000) and end of the 21(st) century climatology (2070-2099) using two models, Geophysical Fluid Dynamics Laboratory (GFDL) model and the Parallel Climate Model (PCM), under the medium-high A2 emission scenario. The digitally mapped results were used to 1) assess the relative redistribution of isobioclimates and their magnitude of change, 2) quantify the loss of isobioclimates into the future, 3) identify and locate novel isobioclimates projected to appear, and 4) explore compositional change in vegetation types among analog isobioclimate patches. This study used downscaled climate variables to map the isobioclimates at a fine spatial resolution -270 m grid cells. Common to both models of future climate was a large change in thermotype. Changes in ombrotype differed among the two models. The end of 20(th) century climatology has 83 isobioclimates covering the 63,000 km(2) study area. In both future projections 51 of those isobioclimates disappear over 40,000 km(2). The ordination of vegetation-bioclimate relationships shows very strong correlation of Rivas-Martinez indices with vegetation distribution and composition. Comparisons of vegetation composition among analog patches suggest that vegetation change will be a local rearrangement of species already in place rather than one requiring long distance dispersal. The digitally mapped results facilitate comparison with other Mediterranean regions. Major remaining challenges include predicting vegetation composition of novel isobioclimates and developing metrics to compare differences in climate space.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>23526985</pmid><doi>10.1371/journal.pone.0058450</doi><tpages>e58450</tpages><oa>free_for_read</oa></addata></record>