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description Publicationkeyboard_double_arrow_right Article , Journal 2012 United StatesPublisher:Oxford University Press (OUP) Authors:Matthew A. Vadeboncoeur;
Steven P. Hamburg; Anne M. Socci; Lynn M. Christenson; +18 AuthorsMatthew A. Vadeboncoeur
Matthew A. Vadeboncoeur in OpenAIREMatthew A. Vadeboncoeur;
Steven P. Hamburg; Anne M. Socci; Lynn M. Christenson;Matthew A. Vadeboncoeur
Matthew A. Vadeboncoeur in OpenAIRECharles T. Driscoll;
Nicholas L. Rodenhouse; Melanie C. Fisk; M. J. Mitchell;Charles T. Driscoll
Charles T. Driscoll in OpenAIRELinda H. Pardo;
Geoffrey W. Wilson; Peter M. Groffman; Paul G. Schaberg;Linda H. Pardo
Linda H. Pardo in OpenAIREChristine L. Goodale;
Christine L. Goodale
Christine L. Goodale in OpenAIREJennifer L. Morse;
Jennifer L. Morse
Jennifer L. Morse in OpenAIREMark B. Green;
Mark B. Green; Pamela H. Templer;Mark B. Green
Mark B. Green in OpenAIRENina K. Lany;
Nina K. Lany
Nina K. Lany in OpenAIREL. Rustad;
Timothy J. Fahey;L. Rustad
L. Rustad in OpenAIREJohn Campbell;
John Campbell
John Campbell in OpenAIREChris E. Johnson;
Chris E. Johnson
Chris E. Johnson in OpenAIREEvaluations of the local effects of global change are often confounded by the interactions of natural and anthropogenic factors that overshadow the effects of climate changes on ecosystems. Long-term watershed and natural elevation gradient studies at the Hubbard Brook Experimental Forest and in the surrounding region show surprising results demonstrating the effects of climate change on hydrologic variables (e.g., evapo- transpiration, streamflow, soil moisture); the importance of changes in phenology on water, carbon, and nitrogen fluxes during critical seasonal transition periods; winter climate change effects on plant and animal community composition and ecosystem services; and the effects of anthro- pogenic disturbances and land-use history on plant community composition. These studies highlight the value of long-term integrated research for assessments of the subtle effects of changing climate on complex ecosystems. unraveling this daunting complexity is long-term studies, including those in which natural elevation gradients are exploited, as a foundation for detailed studies of critical and often unexpected climate-induced changes in forest struc- ture and function. In this article, results from the Hubbard Brook Experimental Forest (HBEF) and the surrounding region are used to illustrate how long-term studies can serve as a foundation for addressing the complex interactions that ultimately determine the effects of climate change on ecosystems. We combine data from long-term (50-year) measurements of multiple aspects of climate and ecosystem structure and function to highlight important but poorly studied inter- actions that could be critical determinants of the responses of plant and animal communities, fluxes of water, element dynamics, and services in northern hardwood forest eco- systems. Our objective is to demonstrate how a combina- tion of long-term and in-depth measurements facilitates A dominant approach in climate change research has been to focus on the effects of changes in temperature and precipitation on broadscale ecosystem properties over large areas and long periods. This body of research suggests that climate change will substantially alter the distribution of species and the function of ecosystems (e.g., Iverson and Prasad 2001), with important effects on ecosystem services. These analyses are based on well-described effects of tem- perature and precipitation on the distribution and activity of organisms. However, climate change is playing out over the complex and dynamic hydrobiogeological structure of the landscape—that is, the intertwined patterns of soils, vegetation, and hydrologic flowpaths, with a spatially variable history of land use and a wide range of current human activities and concurrent environmental changes. The climate effects on ecosystem structure and function may be modified by interactions with these patterns and histories over a range of time scales. We assert that a key approach to
BioScience arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)Portland State University: PDXScholarArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1525/bio.2012.62.12.7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 122 citations 122 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!
more_vert BioScience arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)Portland State University: PDXScholarArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1525/bio.2012.62.12.7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2012 United StatesPublisher:Oxford University Press (OUP) Authors:Matthew A. Vadeboncoeur;
Steven P. Hamburg; Anne M. Socci; Lynn M. Christenson; +18 AuthorsMatthew A. Vadeboncoeur
Matthew A. Vadeboncoeur in OpenAIREMatthew A. Vadeboncoeur;
Steven P. Hamburg; Anne M. Socci; Lynn M. Christenson;Matthew A. Vadeboncoeur
Matthew A. Vadeboncoeur in OpenAIRECharles T. Driscoll;
Nicholas L. Rodenhouse; Melanie C. Fisk; M. J. Mitchell;Charles T. Driscoll
Charles T. Driscoll in OpenAIRELinda H. Pardo;
Geoffrey W. Wilson; Peter M. Groffman; Paul G. Schaberg;Linda H. Pardo
Linda H. Pardo in OpenAIREChristine L. Goodale;
Christine L. Goodale
Christine L. Goodale in OpenAIREJennifer L. Morse;
Jennifer L. Morse
Jennifer L. Morse in OpenAIREMark B. Green;
Mark B. Green; Pamela H. Templer;Mark B. Green
Mark B. Green in OpenAIRENina K. Lany;
Nina K. Lany
Nina K. Lany in OpenAIREL. Rustad;
Timothy J. Fahey;L. Rustad
L. Rustad in OpenAIREJohn Campbell;
John Campbell
John Campbell in OpenAIREChris E. Johnson;
Chris E. Johnson
Chris E. Johnson in OpenAIREEvaluations of the local effects of global change are often confounded by the interactions of natural and anthropogenic factors that overshadow the effects of climate changes on ecosystems. Long-term watershed and natural elevation gradient studies at the Hubbard Brook Experimental Forest and in the surrounding region show surprising results demonstrating the effects of climate change on hydrologic variables (e.g., evapo- transpiration, streamflow, soil moisture); the importance of changes in phenology on water, carbon, and nitrogen fluxes during critical seasonal transition periods; winter climate change effects on plant and animal community composition and ecosystem services; and the effects of anthro- pogenic disturbances and land-use history on plant community composition. These studies highlight the value of long-term integrated research for assessments of the subtle effects of changing climate on complex ecosystems. unraveling this daunting complexity is long-term studies, including those in which natural elevation gradients are exploited, as a foundation for detailed studies of critical and often unexpected climate-induced changes in forest struc- ture and function. In this article, results from the Hubbard Brook Experimental Forest (HBEF) and the surrounding region are used to illustrate how long-term studies can serve as a foundation for addressing the complex interactions that ultimately determine the effects of climate change on ecosystems. We combine data from long-term (50-year) measurements of multiple aspects of climate and ecosystem structure and function to highlight important but poorly studied inter- actions that could be critical determinants of the responses of plant and animal communities, fluxes of water, element dynamics, and services in northern hardwood forest eco- systems. Our objective is to demonstrate how a combina- tion of long-term and in-depth measurements facilitates A dominant approach in climate change research has been to focus on the effects of changes in temperature and precipitation on broadscale ecosystem properties over large areas and long periods. This body of research suggests that climate change will substantially alter the distribution of species and the function of ecosystems (e.g., Iverson and Prasad 2001), with important effects on ecosystem services. These analyses are based on well-described effects of tem- perature and precipitation on the distribution and activity of organisms. However, climate change is playing out over the complex and dynamic hydrobiogeological structure of the landscape—that is, the intertwined patterns of soils, vegetation, and hydrologic flowpaths, with a spatially variable history of land use and a wide range of current human activities and concurrent environmental changes. The climate effects on ecosystem structure and function may be modified by interactions with these patterns and histories over a range of time scales. We assert that a key approach to
BioScience arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)Portland State University: PDXScholarArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1525/bio.2012.62.12.7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 122 citations 122 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!
more_vert BioScience arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)Portland State University: PDXScholarArticle . 2012Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1525/bio.2012.62.12.7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2016 United StatesPublisher:Wiley Authors:William H. McDowell;
William H. McDowell
William H. McDowell in OpenAIREAlexandra R. Contosta;
Alexandra R. Contosta
Alexandra R. Contosta in OpenAIRECameron P. Wake;
Mary R. Albert; +11 AuthorsCameron P. Wake
Cameron P. Wake in OpenAIREWilliam H. McDowell;
William H. McDowell
William H. McDowell in OpenAIREAlexandra R. Contosta;
Alexandra R. Contosta
Alexandra R. Contosta in OpenAIRECameron P. Wake;
Mary R. Albert;Cameron P. Wake
Cameron P. Wake in OpenAIREA. C. Adolph;
Denise Burchsted;A. C. Adolph
A. C. Adolph in OpenAIREElizabeth A. Burakowski;
Elizabeth A. Burakowski;Elizabeth A. Burakowski
Elizabeth A. Burakowski in OpenAIREWilfred M. Wollheim;
David Guerra;Wilfred M. Wollheim
Wilfred M. Wollheim in OpenAIREMark B. Green;
Jack E. Dibb; Rachel J. Whitaker; Mary E. Martin; Michael R. Routhier;Mark B. Green
Mark B. Green in OpenAIREdoi: 10.1111/gcb.13517
pmid: 27808458
AbstractClimate change is altering the timing and duration of the vernal window, a period that marks the end of winter and the start of the growing season when rapid transitions in ecosystem energy, water, nutrient, and carbon dynamics take place. Research on this period typically captures only a portion of the ecosystem in transition and focuses largely on the dates by which the system wakes up. Previous work has not addressed lags between transitions that represent delays in energy, water, nutrient, and carbon flows. The objectives of this study were to establish the sequence of physical and biogeochemical transitions and lags during the vernal window period and to understand how climate change may alter them. We synthesized observations from a statewide sensor network in New Hampshire,USA, that concurrently monitored climate, snow, soils, and streams over a three‐year period and supplemented these observations with climate reanalysis data, snow data assimilation model output, and satellite spectral data. We found that some of the transitions that occurred within the vernal window were sequential, with air temperatures warming prior to snow melt, which preceded forest canopy closure. Other transitions were simultaneous with one another and had zero‐length lags, such as snowpack disappearance, rapid soil warming, and peak stream discharge. We modeled lags as a function of both winter coldness and snow depth, both of which are expected to decline with climate change. Warmer winters with less snow resulted in longer lags and a more protracted vernal window. This lengthening of individual lags and of the entire vernal window carries important consequences for the thermodynamics and biogeochemistry of ecosystems, both during the winter‐to‐spring transition and throughout the rest of the year.
University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BY NC NDFull-Text: https://scholars.unh.edu/ersc/43Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.13517&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 59 citations 59 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
more_vert University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BY NC NDFull-Text: https://scholars.unh.edu/ersc/43Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.13517&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2016 United StatesPublisher:Wiley Authors:William H. McDowell;
William H. McDowell
William H. McDowell in OpenAIREAlexandra R. Contosta;
Alexandra R. Contosta
Alexandra R. Contosta in OpenAIRECameron P. Wake;
Mary R. Albert; +11 AuthorsCameron P. Wake
Cameron P. Wake in OpenAIREWilliam H. McDowell;
William H. McDowell
William H. McDowell in OpenAIREAlexandra R. Contosta;
Alexandra R. Contosta
Alexandra R. Contosta in OpenAIRECameron P. Wake;
Mary R. Albert;Cameron P. Wake
Cameron P. Wake in OpenAIREA. C. Adolph;
Denise Burchsted;A. C. Adolph
A. C. Adolph in OpenAIREElizabeth A. Burakowski;
Elizabeth A. Burakowski;Elizabeth A. Burakowski
Elizabeth A. Burakowski in OpenAIREWilfred M. Wollheim;
David Guerra;Wilfred M. Wollheim
Wilfred M. Wollheim in OpenAIREMark B. Green;
Jack E. Dibb; Rachel J. Whitaker; Mary E. Martin; Michael R. Routhier;Mark B. Green
Mark B. Green in OpenAIREdoi: 10.1111/gcb.13517
pmid: 27808458
AbstractClimate change is altering the timing and duration of the vernal window, a period that marks the end of winter and the start of the growing season when rapid transitions in ecosystem energy, water, nutrient, and carbon dynamics take place. Research on this period typically captures only a portion of the ecosystem in transition and focuses largely on the dates by which the system wakes up. Previous work has not addressed lags between transitions that represent delays in energy, water, nutrient, and carbon flows. The objectives of this study were to establish the sequence of physical and biogeochemical transitions and lags during the vernal window period and to understand how climate change may alter them. We synthesized observations from a statewide sensor network in New Hampshire,USA, that concurrently monitored climate, snow, soils, and streams over a three‐year period and supplemented these observations with climate reanalysis data, snow data assimilation model output, and satellite spectral data. We found that some of the transitions that occurred within the vernal window were sequential, with air temperatures warming prior to snow melt, which preceded forest canopy closure. Other transitions were simultaneous with one another and had zero‐length lags, such as snowpack disappearance, rapid soil warming, and peak stream discharge. We modeled lags as a function of both winter coldness and snow depth, both of which are expected to decline with climate change. Warmer winters with less snow resulted in longer lags and a more protracted vernal window. This lengthening of individual lags and of the entire vernal window carries important consequences for the thermodynamics and biogeochemistry of ecosystems, both during the winter‐to‐spring transition and throughout the rest of the year.
University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BY NC NDFull-Text: https://scholars.unh.edu/ersc/43Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.13517&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 59 citations 59 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
more_vert University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BY NC NDFull-Text: https://scholars.unh.edu/ersc/43Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.13517&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal 2014 United StatesPublisher:Wiley Funded by:NSERCNSERCAuthors:Creed, Irena F;
Spargo, Adam T; Jones, Julia A.; Buttle, Jim M; +17 AuthorsCreed, Irena F
Creed, Irena F in OpenAIRECreed, Irena F;
Spargo, Adam T; Jones, Julia A.; Buttle, Jim M;Creed, Irena F
Creed, Irena F in OpenAIREAdams, Mary B;
Beall, Fred D;Adams, Mary B
Adams, Mary B in OpenAIREBooth, Eric G;
Booth, Eric G
Booth, Eric G in OpenAIRECampbell, John L;
Clow, Dave; Elder, Kelly;Campbell, John L
Campbell, John L in OpenAIREGreen, Mark B;
Green, Mark B
Green, Mark B in OpenAIREGrimm, Nancy B;
Grimm, Nancy B
Grimm, Nancy B in OpenAIREMiniat, Chelcy;
Ramlal, Patricia; Saha, Amartya;Miniat, Chelcy
Miniat, Chelcy in OpenAIRESebestyen, Stephen;
Spittlehouse, Dave; Sterling, Shannon; Williams, Mark W; Wrinkler, Rita;Sebestyen, Stephen
Sebestyen, Stephen in OpenAIREYao, Huaxia;
Yao, Huaxia
Yao, Huaxia in OpenAIREAbstractClimate warming is projected to affect forest water yields but the effects are expected to vary. We investigated how forest type and age affect water yield resilience to climate warming. To answer this question, we examined the variability in historical water yields at long‐term experimental catchments across Canada and the United States over 5‐year cool and warm periods. Using the theoretical framework of the Budyko curve, we calculated the effects of climate warming on the annual partitioning of precipitation (P) into evapotranspiration (ET) and water yield. Deviation (d) was defined as a catchment's change in actual ET divided by P [AET/P; evaporative index (EI)] coincident with a shift from a cool to a warm period – a positive d indicates an upward shift in EI and smaller than expected water yields, and a negative d indicates a downward shift in EI and larger than expected water yields. Elasticity was defined as the ratio of interannual variation in potential ET divided by P (PET/P; dryness index) to interannual variation in the EI – high elasticity indicates low d despite large range in drying index (i.e., resilient water yields), low elasticity indicates high d despite small range in drying index (i.e., nonresilient water yields). Although the data needed to fully evaluate ecosystems based on these metrics are limited, we were able to identify some characteristics of response among forest types. Alpine sites showed the greatest sensitivity to climate warming with any warming leading to increased water yields. Conifer forests included catchments with lowest elasticity and stable to larger water yields. Deciduous forests included catchments with intermediate elasticity and stable to smaller water yields. Mixed coniferous/deciduous forests included catchments with highest elasticity and stable water yields. Forest type appeared to influence the resilience of catchment water yields to climate warming, with conifer and deciduous catchments more susceptible to climate warming than the more diverse mixed forest catchments.
University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2014License: CC BYFull-Text: https://scholars.unh.edu/nh_epscor/216Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.12615&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 159 citations 159 popularity Top 1% influence Top 10% impulse Top 10% Powered by BIP!
more_vert University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2014License: CC BYFull-Text: https://scholars.unh.edu/nh_epscor/216Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.12615&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal 2014 United StatesPublisher:Wiley Funded by:NSERCNSERCAuthors:Creed, Irena F;
Spargo, Adam T; Jones, Julia A.; Buttle, Jim M; +17 AuthorsCreed, Irena F
Creed, Irena F in OpenAIRECreed, Irena F;
Spargo, Adam T; Jones, Julia A.; Buttle, Jim M;Creed, Irena F
Creed, Irena F in OpenAIREAdams, Mary B;
Beall, Fred D;Adams, Mary B
Adams, Mary B in OpenAIREBooth, Eric G;
Booth, Eric G
Booth, Eric G in OpenAIRECampbell, John L;
Clow, Dave; Elder, Kelly;Campbell, John L
Campbell, John L in OpenAIREGreen, Mark B;
Green, Mark B
Green, Mark B in OpenAIREGrimm, Nancy B;
Grimm, Nancy B
Grimm, Nancy B in OpenAIREMiniat, Chelcy;
Ramlal, Patricia; Saha, Amartya;Miniat, Chelcy
Miniat, Chelcy in OpenAIRESebestyen, Stephen;
Spittlehouse, Dave; Sterling, Shannon; Williams, Mark W; Wrinkler, Rita;Sebestyen, Stephen
Sebestyen, Stephen in OpenAIREYao, Huaxia;
Yao, Huaxia
Yao, Huaxia in OpenAIREAbstractClimate warming is projected to affect forest water yields but the effects are expected to vary. We investigated how forest type and age affect water yield resilience to climate warming. To answer this question, we examined the variability in historical water yields at long‐term experimental catchments across Canada and the United States over 5‐year cool and warm periods. Using the theoretical framework of the Budyko curve, we calculated the effects of climate warming on the annual partitioning of precipitation (P) into evapotranspiration (ET) and water yield. Deviation (d) was defined as a catchment's change in actual ET divided by P [AET/P; evaporative index (EI)] coincident with a shift from a cool to a warm period – a positive d indicates an upward shift in EI and smaller than expected water yields, and a negative d indicates a downward shift in EI and larger than expected water yields. Elasticity was defined as the ratio of interannual variation in potential ET divided by P (PET/P; dryness index) to interannual variation in the EI – high elasticity indicates low d despite large range in drying index (i.e., resilient water yields), low elasticity indicates high d despite small range in drying index (i.e., nonresilient water yields). Although the data needed to fully evaluate ecosystems based on these metrics are limited, we were able to identify some characteristics of response among forest types. Alpine sites showed the greatest sensitivity to climate warming with any warming leading to increased water yields. Conifer forests included catchments with lowest elasticity and stable to larger water yields. Deciduous forests included catchments with intermediate elasticity and stable to smaller water yields. Mixed coniferous/deciduous forests included catchments with highest elasticity and stable water yields. Forest type appeared to influence the resilience of catchment water yields to climate warming, with conifer and deciduous catchments more susceptible to climate warming than the more diverse mixed forest catchments.
University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2014License: CC BYFull-Text: https://scholars.unh.edu/nh_epscor/216Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.12615&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 159 citations 159 popularity Top 1% influence Top 10% impulse Top 10% Powered by BIP!
more_vert University of New Ha... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2014License: CC BYFull-Text: https://scholars.unh.edu/nh_epscor/216Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1111/gcb.12615&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2013 United StatesPublisher:Proceedings of the National Academy of Sciences Authors: Amey S. Bailey; Paul G. Schaberg;John J. Battles;
John J. Battles
John J. Battles in OpenAIRECharles T. Driscoll;
+8 AuthorsCharles T. Driscoll
Charles T. Driscoll in OpenAIREAmey S. Bailey; Paul G. Schaberg;John J. Battles;
John J. Battles
John J. Battles in OpenAIRECharles T. Driscoll;
Charles T. Driscoll
Charles T. Driscoll in OpenAIREMark B. Green;
Mark B. Green
Mark B. Green in OpenAIREScott W. Bailey;
Gene E. Likens; Gene E. Likens; Timothy J. Fahey;Scott W. Bailey
Scott W. Bailey in OpenAIREScott V. Ollinger;
Scott V. Ollinger
Scott V. Ollinger in OpenAIREJohn Campbell;
John Campbell
John Campbell in OpenAIRELucie C. Lepine;
Lucie C. Lepine
Lucie C. Lepine in OpenAIREAcid deposition during the 20th century caused widespread depletion of available soil calcium (Ca) throughout much of the industrialized world. To better understand how forest ecosystems respond to changes in a component of acidification stress, an 11.8-ha watershed was amended with wollastonite, a calcium silicate mineral, to restore available soil Ca to preindustrial levels through natural weathering. An unexpected outcome of the Ca amendment was a change in watershed hydrology; annual evapotranspiration increased by 25%, 18%, and 19%, respectively, for the 3 y following treatment before returning to pretreatment levels. During this period, the watershed retained Ca from the wollastonite, indicating a watershed-scale fertilization effect on transpiration. That response is unique in being a measured manipulation of watershed runoff attributable to fertilization, a response of similar magnitude to effects of deforestation. Our results suggest that past and future changes in available soil Ca concentrations have important and previously unrecognized implications for the water cycle.
Proceedings of the N... arrow_drop_down Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefUniversity of New Hampshire: Scholars RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1302445110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 45 citations 45 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
more_vert Proceedings of the N... arrow_drop_down Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefUniversity of New Hampshire: Scholars RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1302445110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2013 United StatesPublisher:Proceedings of the National Academy of Sciences Authors: Amey S. Bailey; Paul G. Schaberg;John J. Battles;
John J. Battles
John J. Battles in OpenAIRECharles T. Driscoll;
+8 AuthorsCharles T. Driscoll
Charles T. Driscoll in OpenAIREAmey S. Bailey; Paul G. Schaberg;John J. Battles;
John J. Battles
John J. Battles in OpenAIRECharles T. Driscoll;
Charles T. Driscoll
Charles T. Driscoll in OpenAIREMark B. Green;
Mark B. Green
Mark B. Green in OpenAIREScott W. Bailey;
Gene E. Likens; Gene E. Likens; Timothy J. Fahey;Scott W. Bailey
Scott W. Bailey in OpenAIREScott V. Ollinger;
Scott V. Ollinger
Scott V. Ollinger in OpenAIREJohn Campbell;
John Campbell
John Campbell in OpenAIRELucie C. Lepine;
Lucie C. Lepine
Lucie C. Lepine in OpenAIREAcid deposition during the 20th century caused widespread depletion of available soil calcium (Ca) throughout much of the industrialized world. To better understand how forest ecosystems respond to changes in a component of acidification stress, an 11.8-ha watershed was amended with wollastonite, a calcium silicate mineral, to restore available soil Ca to preindustrial levels through natural weathering. An unexpected outcome of the Ca amendment was a change in watershed hydrology; annual evapotranspiration increased by 25%, 18%, and 19%, respectively, for the 3 y following treatment before returning to pretreatment levels. During this period, the watershed retained Ca from the wollastonite, indicating a watershed-scale fertilization effect on transpiration. That response is unique in being a measured manipulation of watershed runoff attributable to fertilization, a response of similar magnitude to effects of deforestation. Our results suggest that past and future changes in available soil Ca concentrations have important and previously unrecognized implications for the water cycle.
Proceedings of the N... arrow_drop_down Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefUniversity of New Hampshire: Scholars RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1302445110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 45 citations 45 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
more_vert Proceedings of the N... arrow_drop_down Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefUniversity of New Hampshire: Scholars RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1302445110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu