Complex responses to climate drivers in onset of spring flowering across a semi-arid elevation gradient

1. Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water-limited environment may respond to predicted changes in climate, we used a speci...

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Published inThe Journal of ecology Vol. 98; no. 5; pp. 1042 - 1051
Main Authors Crimmins, Theresa M, Crimmins, Michael A, David Bertelsen, C
Format Journal Article
LanguageEnglish
Published Oxford, UK Oxford, UK : Blackwell Publishing Ltd 01.09.2010
Blackwell Publishing
Blackwell Publishing Ltd
Blackwell
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Abstract 1. Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water-limited environment may respond to predicted changes in climate, we used a species-rich 20-year data set collected in a semi-arid ecosystem to determine species' relationships with precipitation and temperature for seasons coincident with and previous to flowering. Our data were collected across a 1200-m elevation gradient, allowing us to explore the consistency in relationships with climatic variables from desert scrub to pine forest. A second objective was to document evidence of changes in the onset of spring flowering over this 20-year period. 2. Onset of spring flowering for species at the lowest elevations was most commonly driven by temperature and precipitation conditions of the previous autumn. In contrast, onset of spring flowering for species in high-elevation communities was more often associated with spring temperatures, a pattern consistent with communities of higher latitudes. Despite these coarse patterns, species' relationships to climate variables were highly variable and individualistic. 3. Approximately 10% of species showed a significant trend in changes in first flowering date over the period 1984-2003; most trends were in the direction of later onset. The decrease in autumn precipitation observed over the study period appears to explain the delay in onset observed for many of the species across the elevation gradient. Other species' delays in spring flowering appear to be related to the slight decrease in spring temperature observed over the study period. 4. Synthesis. The south-western USA is expected to become warmer and drier. Climate relationships documented in this study suggest divergent, individualistic changes in the onset of spring flowering. Low-elevation plants may exhibit delayed spring flowering due to changes in the timing or amount of precipitation or insufficient chilling. High-elevation species may show advancement in spring flowering due to warming temperatures. The highly individualistic responses to climate change may result in significant changes in the diversity, composition and abundance of plants in flower. Variable changes in phenology such as these have major implications for species population dynamics and ecosystem functioning.
AbstractList 1. Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water-limited environment may respond to predicted changes in climate, we used a species-rich 20-year data set collected in a semi-arid ecosystem to determine species' relationships with precipitation and temperature for seasons coincident with and previous to flowering. Our data were collected across a 1200-m elevation gradient, allowing us to explore the consistency in relationships with climatic variables from desert scrub to pine forest. A second objective was to document evidence of changes in the onset of spring flowering over this 20-year period. 2. Onset of spring flowering for species at the lowest elevations was most commonly driven by temperature and precipitation conditions of the previous autumn. In contrast, onset of spring flowering for species in high-elevation communities was more often associated with spring temperatures, a pattern consistent with communities of higher latitudes. Despite these coarse patterns, species' relationships to climate variables were highly variable and individualistic. 3. Approximately 10% of species showed a significant trend in changes in first flowering date over the period 1984-2003; most trends were in the direction of later onset. The decrease in autumn precipitation observed over the study period appears to explain the delay in onset observed for many of the species across the elevation gradient. Other species' delays in spring flowering appear to be related to the slight decrease in spring temperature observed over the study period. 4. Synthesis. The south-western USA is expected to become warmer and drier. Climate relationships documented in this study suggest divergent, individualistic changes in the onset of spring flowering. Low-elevation plants may exhibit delayed spring flowering due to changes in the timing or amount of precipitation or insufficient chilling. High-elevation species may show advancement in spring flowering due to warming temperatures. The highly individualistic responses to climate change may result in significant changes in the diversity, composition and abundance of plants in flower. Variable changes in phenology such as these have major implications for species population dynamics and ecosystem functioning.
Summary 1.  Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water‐limited environment may respond to predicted changes in climate, we used a species‐rich 20‐year data set collected in a semi‐arid ecosystem to determine species’ relationships with precipitation and temperature for seasons coincident with and previous to flowering. Our data were collected across a 1200‐m elevation gradient, allowing us to explore the consistency in relationships with climatic variables from desert scrub to pine forest. A second objective was to document evidence of changes in the onset of spring flowering over this 20‐year period. 2.  Onset of spring flowering for species at the lowest elevations was most commonly driven by temperature and precipitation conditions of the previous autumn. In contrast, onset of spring flowering for species in high‐elevation communities was more often associated with spring temperatures, a pattern consistent with communities of higher latitudes. Despite these coarse patterns, species’ relationships to climate variables were highly variable and individualistic. 3.  Approximately 10% of species showed a significant trend in changes in first flowering date over the period 1984–2003; most trends were in the direction of later onset. The decrease in autumn precipitation observed over the study period appears to explain the delay in onset observed for many of the species across the elevation gradient. Other species’ delays in spring flowering appear to be related to the slight decrease in spring temperature observed over the study period. 4.   Synthesis. The south‐western USA is expected to become warmer and drier. Climate relationships documented in this study suggest divergent, individualistic changes in the onset of spring flowering. Low‐elevation plants may exhibit delayed spring flowering due to changes in the timing or amount of precipitation or insufficient chilling. High‐elevation species may show advancement in spring flowering due to warming temperatures. The highly individualistic responses to climate change may result in significant changes in the diversity, composition and abundance of plants in flower. Variable changes in phenology such as these have major implications for species population dynamics and ecosystem functioning.
Summary 1. Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water‐limited environment may respond to predicted changes in climate, we used a species‐rich 20‐year data set collected in a semi‐arid ecosystem to determine species’ relationships with precipitation and temperature for seasons coincident with and previous to flowering. Our data were collected across a 1200‐m elevation gradient, allowing us to explore the consistency in relationships with climatic variables from desert scrub to pine forest. A second objective was to document evidence of changes in the onset of spring flowering over this 20‐year period. 2. Onset of spring flowering for species at the lowest elevations was most commonly driven by temperature and precipitation conditions of the previous autumn. In contrast, onset of spring flowering for species in high‐elevation communities was more often associated with spring temperatures, a pattern consistent with communities of higher latitudes. Despite these coarse patterns, species’ relationships to climate variables were highly variable and individualistic. 3. Approximately 10% of species showed a significant trend in changes in first flowering date over the period 1984–2003; most trends were in the direction of later onset. The decrease in autumn precipitation observed over the study period appears to explain the delay in onset observed for many of the species across the elevation gradient. Other species’ delays in spring flowering appear to be related to the slight decrease in spring temperature observed over the study period. 4. Synthesis. The south‐western USA is expected to become warmer and drier. Climate relationships documented in this study suggest divergent, individualistic changes in the onset of spring flowering. Low‐elevation plants may exhibit delayed spring flowering due to changes in the timing or amount of precipitation or insufficient chilling. High‐elevation species may show advancement in spring flowering due to warming temperatures. The highly individualistic responses to climate change may result in significant changes in the diversity, composition and abundance of plants in flower. Variable changes in phenology such as these have major implications for species population dynamics and ecosystem functioning.
Summary1.Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water-limited environment may respond to predicted changes in climate, we used a species-rich 20-year data set collected in a semi-arid ecosystem to determine species' relationships with precipitation and temperature for seasons coincident with and previous to flowering. Our data were collected across a 1200-m elevation gradient, allowing us to explore the consistency in relationships with climatic variables from desert scrub to pine forest. A second objective was to document evidence of changes in the onset of spring flowering over this 20-year period.2.Onset of spring flowering for species at the lowest elevations was most commonly driven by temperature and precipitation conditions of the previous autumn. In contrast, onset of spring flowering for species in high-elevation communities was more often associated with spring temperatures, a pattern consistent with communities of higher latitudes. Despite these coarse patterns, species' relationships to climate variables were highly variable and individualistic.3.Approximately 10% of species showed a significant trend in changes in first flowering date over the period 1984-2003; most trends were in the direction of later onset. The decrease in autumn precipitation observed over the study period appears to explain the delay in onset observed for many of the species across the elevation gradient. Other species' delays in spring flowering appear to be related to the slight decrease in spring temperature observed over the study period.4.Synthesis. The south-western USA is expected to become warmer and drier. Climate relationships documented in this study suggest divergent, individualistic changes in the onset of spring flowering. Low-elevation plants may exhibit delayed spring flowering due to changes in the timing or amount of precipitation or insufficient chilling. High-elevation species may show advancement in spring flowering due to warming temperatures. The highly individualistic responses to climate change may result in significant changes in the diversity, composition and abundance of plants in flower. Variable changes in phenology such as these have major implications for species population dynamics and ecosystem functioning.
Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting factor, are rare. To better understand how plants of a water-limited environment may respond to predicted changes in climate, we used a species-rich 20-year data set collected in a semi-arid ecosystem to determine species' relationships with precipitation and temperature for seasons coincident with and previous to flowering. Our data were collected across a 1200-m elevation gradient, allowing us to explore the consistency in relationships with climatic variables from desert scrub to pine forest. A second objective was to document evidence of changes in the onset of spring flowering over this 20-year period. Onset of spring flowering for species at the lowest elevations was most commonly driven by temperature and precipitation conditions of the previous autumn. In contrast, onset of spring flowering for species in high-elevation communities was more often associated with spring temperatures, a pattern consistent with communities of higher latitudes. Despite these coarse patterns, species' relationships to climate variables were highly variable and individualistic. Approximately 10% of species showed a significant trend in changes in first flowering date over the period 1984-2003; most trends were in the direction of later onset. The decrease in autumn precipitation observed over the study period appears to explain the delay in onset observed for many of the species across the elevation gradient. Other species' delays in spring flowering appear to be related to the slight decrease in spring temperature observed over the study period. The south-western USA is expected to become warmer and drier. Climate relationships documented in this study suggest divergent, individualistic changes in the onset of spring flowering. Low-elevation plants may exhibit delayed spring flowering due to changes in the timing or amount of precipitation or insufficient chilling. High-elevation species may show advancement in spring flowering due to warming temperatures. The highly individualistic responses to climate change may result in significant changes in the diversity, composition and abundance of plants in flower. Variable changes in phenology such as these have major implications for species population dynamics and ecosystem functioning.
Author Crimmins, Michael A
Crimmins, Theresa M
David Bertelsen, C
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ID FETCH-LOGICAL-c4986-4485fbec23794f0263ea1ae2460c0d00c0539d938ee170f3b4ebd42865987f773
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ISSN 0022-0477
IngestDate Fri Aug 16 01:11:34 EDT 2024
Thu Oct 10 16:43:33 EDT 2024
Fri Aug 23 00:53:23 EDT 2024
Sun Oct 22 16:03:22 EDT 2023
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Fri Feb 02 07:02:26 EST 2024
Wed Dec 27 19:17:16 EST 2023
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Issue 5
Keywords Climate
first flowering date
Arid environment
Interaction
plant-climate interactions
Dynamical climatology
Climate change
Phenology
Semi arid zone
Flowering
elevation gradient
semi-arid environment
Arizona
Language English
License CC BY 4.0
LinkModel DirectLink
MergedId FETCHMERGED-LOGICAL-c4986-4485fbec23794f0263ea1ae2460c0d00c0539d938ee170f3b4ebd42865987f773
Notes http://dx.doi.org/10.1111/j.1365-2745.2010.01696.x
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content type line 23
OpenAccessLink https://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/j.1365-2745.2010.01696.x
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PublicationTitle The Journal of ecology
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Snippet 1. Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting...
Summary 1. Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the...
Summary 1.  Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the...
Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the limiting...
Summary1.Many studies have documented advancement in spring plant phenology; however, studies in dry climates, where water, rather than temperature, is the...
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SubjectTerms Animal and plant ecology
Animal, plant and microbial ecology
Arizona
Autumn
Biological and medical sciences
Climate change
Climate models
Climatology
Climatology. Bioclimatology. Climate change
Deserts
Earth, ocean, space
Ecology
Ecosystems
elevation gradient
Exact sciences and technology
External geophysics
first flowering date
Flowering
Flowers & plants
Fundamental and applied biological sciences. Psychology
General aspects
Meteorology
Phenology
Plant-climate interactions
Plants
Precipitation
semi-arid environment
Species
Temperature
Title Complex responses to climate drivers in onset of spring flowering across a semi-arid elevation gradient
URI https://www.jstor.org/stable/40929053
https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fj.1365-2745.2010.01696.x
https://www.proquest.com/docview/743880612
https://search.proquest.com/docview/754897254
Volume 98
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