The climate velocity of the contiguous United States during the 20th century

Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of on‐going climate change will exceed the rate at which species can adapt or move to suitable environments. Here we assess the climate velocity (b...

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Published in:Global change biology Vol. 19; no. 1; pp. 241 - 251
Main Authors: Dobrowski, Solomon Z., Abatzoglou, John, Swanson, Alan K., Greenberg, Jonathan A., Mynsberge, Alison R., Holden, Zachary A., Schwartz, Michael K.
Format: Journal Article
Language:English
Published: Oxford Blackwell Publishing Ltd 01.01.2013
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ISSN:1354-1013, 1365-2486
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Abstract Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of on‐going climate change will exceed the rate at which species can adapt or move to suitable environments. Here we assess the climate velocity (both climate displacement rate and direction) for minimum temperature, actual evapotranspiration, and climatic water deficit (deficit) over the contiguous US during the 20th century (1916–2005). Vectors for these variables demonstrate a complex mosaic of patterns that vary spatially and temporally and are dependent on the spatial resolution of input climate data. Velocities for variables that characterize the climatic water balance were similar in magnitude to that derived from temperature, but frequently differed in direction resulting in the divergence of climate vectors through time. Our results strain expectations of poleward and upslope migration over the past century due to warming. Instead, they suggest that a more full understanding of changes in multiple climatic factors, in addition to temperature, may help explain unexpected or conflicting observational evidence of climate‐driven species range shifts during the 20th century.
AbstractList Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of on-going climate change will exceed the rate at which species can adapt or move to suitable environments. Here we assess the climate velocity (both climate displacement rate and direction) for minimum temperature, actual evapotranspiration, and climatic water deficit (deficit) over the contiguous US during the 20th century (1916-2005). Vectors for these variables demonstrate a complex mosaic of patterns that vary spatially and temporally and are dependent on the spatial resolution of input climate data. Velocities for variables that characterize the climatic water balance were similar in magnitude to that derived from temperature, but frequently differed in direction resulting in the divergence of climate vectors through time. Our results strain expectations of poleward and upslope migration over the past century due to warming. Instead, they suggest that a more full understanding of changes in multiple climatic factors, in addition to temperature, may help explain unexpected or conflicting observational evidence of climate-driven species range shifts during the 20th century.Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of on-going climate change will exceed the rate at which species can adapt or move to suitable environments. Here we assess the climate velocity (both climate displacement rate and direction) for minimum temperature, actual evapotranspiration, and climatic water deficit (deficit) over the contiguous US during the 20th century (1916-2005). Vectors for these variables demonstrate a complex mosaic of patterns that vary spatially and temporally and are dependent on the spatial resolution of input climate data. Velocities for variables that characterize the climatic water balance were similar in magnitude to that derived from temperature, but frequently differed in direction resulting in the divergence of climate vectors through time. Our results strain expectations of poleward and upslope migration over the past century due to warming. Instead, they suggest that a more full understanding of changes in multiple climatic factors, in addition to temperature, may help explain unexpected or conflicting observational evidence of climate-driven species range shifts during the 20th century.
Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of on‐going climate change will exceed the rate at which species can adapt or move to suitable environments. Here we assess the climate velocity (both climate displacement rate and direction) for minimum temperature, actual evapotranspiration, and climatic water deficit (deficit) over the contiguous US during the 20th century (1916–2005). Vectors for these variables demonstrate a complex mosaic of patterns that vary spatially and temporally and are dependent on the spatial resolution of input climate data. Velocities for variables that characterize the climatic water balance were similar in magnitude to that derived from temperature, but frequently differed in direction resulting in the divergence of climate vectors through time. Our results strain expectations of poleward and upslope migration over the past century due to warming. Instead, they suggest that a more full understanding of changes in multiple climatic factors, in addition to temperature, may help explain unexpected or conflicting observational evidence of climate‐driven species range shifts during the 20th century.
Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of on-going climate change will exceed the rate at which species can adapt or move to suitable environments. Here we assess the climate velocity (both climate displacement rate and direction) for minimum temperature, actual evapotranspiration, and climatic water deficit (deficit) over the contiguous US during the 20th century (1916-2005). Vectors for these variables demonstrate a complex mosaic of patterns that vary spatially and temporally and are dependent on the spatial resolution of input climate data. Velocities for variables that characterize the climatic water balance were similar in magnitude to that derived from temperature, but frequently differed in direction resulting in the divergence of climate vectors through time. Our results strain expectations of poleward and upslope migration over the past century due to warming. Instead, they suggest that a more full understanding of changes in multiple climatic factors, in addition to temperature, may help explain unexpected or conflicting observational evidence of climate-driven species range shifts during the 20th century. [PUBLICATION ABSTRACT]
Author Greenberg, Jonathan A.
Swanson, Alan K.
Abatzoglou, John
Holden, Zachary A.
Dobrowski, Solomon Z.
Mynsberge, Alison R.
Schwartz, Michael K.
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  organization: U.S. Forest Service, Rocky Mountain Research Station, Missoula, MT 59801, USA
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Issue 1
Keywords Dynamical climatology
Climatic condition
Climate change
Climate
climate change velocity
climatic water balance
climate change impacts
Environmental factor
Water balance
Vector
climate velocity vectors
Language English
License CC BY 4.0
2012 Blackwell Publishing Ltd.
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Notes National Science Foundation - No. 0814387; No. 0819430
USDA Forest Service Rocky Mountain Research Station - No. JV11221635-201
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USDA CSREES - No. 2008-38420-19524
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Appendix A. Detailed methods for water balance model.Appendix B. Code for replicating water balance calculations in R.Appendix C. Validation of climate gradients used in water balance model.
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Snippet Rapid climate change has the potential to affect economic, social, and biological systems. A concern for species conservation is whether or not the rate of...
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SubjectTerms Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Climate Change
climate change impacts
climate change velocity
climate velocity vectors
Climatic data
climatic factors
climatic water balance
Climatology. Bioclimatology. Climate change
Conservation biology
Earth, ocean, space
economics
Evapotranspiration
Exact sciences and technology
External geophysics
Fundamental and applied biological sciences. Psychology
General aspects
Global warming
History, 20th Century
Meteorology
temperature
United States
Water balance
Water deficit
Title The climate velocity of the contiguous United States during the 20th century
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Volume 19
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