Are the impacts of land use on warming underestimated in climate policy?

While carbon dioxide emissions from energy use must be the primary target of climate change mitigation efforts, land use and land cover change (LULCC) also represent an important source of climate forcing. In this study we compute time series of global surface temperature change separately for LULCC...

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Main Authors: Natalie M Mahowald, Daniel S Ward, Scott C Doney, Peter G Hess, James T Randerson
Format: Article
Language:English
Published: IOP Publishing 2017-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aa836d
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author Natalie M Mahowald
Daniel S Ward
Scott C Doney
Peter G Hess
James T Randerson
author_facet Natalie M Mahowald
Daniel S Ward
Scott C Doney
Peter G Hess
James T Randerson
author_sort Natalie M Mahowald
collection DOAJ
description While carbon dioxide emissions from energy use must be the primary target of climate change mitigation efforts, land use and land cover change (LULCC) also represent an important source of climate forcing. In this study we compute time series of global surface temperature change separately for LULCC and non-LULCC sources (primarily fossil fuel burning), and show that because of the extra warming associated with the co-emission of methane and nitrous oxide with LULCC carbon dioxide emissions, and a co-emission of cooling aerosols with non-LULCC emissions of carbon dioxide, the linear relationship between cumulative carbon dioxide emissions and temperature has a two-fold higher slope for LULCC than for non-LULCC activities. Moreover, projections used in the Intergovernmental Panel on Climate Change (IPCC) for the rate of tropical land conversion in the future are relatively low compared to contemporary observations, suggesting that the future projections of land conversion used in the IPCC may underestimate potential impacts of LULCC. By including a ‘business as usual’ future LULCC scenario for tropical deforestation, we find that even if all non-LULCC emissions are switched off in 2015, it is likely that 1.5 °C of warming relative to the preindustrial era will occur by 2100. Thus, policies to reduce LULCC emissions must remain a high priority if we are to achieve the low to medium temperature change targets proposed as a part of the Paris Agreement. Future studies using integrated assessment models and other climate simulations should include more realistic deforestation rates and the integration of policy that would reduce LULCC emissions.
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spelling doaj.art-d31df3f61d684333861a8ed633b6e1942023-08-09T14:36:33ZengIOP PublishingEnvironmental Research Letters1748-93262017-01-0112909401610.1088/1748-9326/aa836dAre the impacts of land use on warming underestimated in climate policy?Natalie M Mahowald0Daniel S Ward1Scott C Doney2Peter G Hess3James T Randerson4Department of Earth and Atmospheric Sciences, Atkinson Center for a Sustainable Future , Cornell University, Ithaca, NY, United States of America; Author to whom any correspondence should be addressed.Program in Atmospheric and Oceanic Sciences , Princeton University, Princeton, NJ, United States of AmericaMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution , Woods Hole, MA, United States of AmericaDepartment of Biological and Environmental Engineering , Cornell University, Ithaca, NY, United States of AmericaDepartment of Earth System Science , University of California, Irvine, CA, United States of AmericaWhile carbon dioxide emissions from energy use must be the primary target of climate change mitigation efforts, land use and land cover change (LULCC) also represent an important source of climate forcing. In this study we compute time series of global surface temperature change separately for LULCC and non-LULCC sources (primarily fossil fuel burning), and show that because of the extra warming associated with the co-emission of methane and nitrous oxide with LULCC carbon dioxide emissions, and a co-emission of cooling aerosols with non-LULCC emissions of carbon dioxide, the linear relationship between cumulative carbon dioxide emissions and temperature has a two-fold higher slope for LULCC than for non-LULCC activities. Moreover, projections used in the Intergovernmental Panel on Climate Change (IPCC) for the rate of tropical land conversion in the future are relatively low compared to contemporary observations, suggesting that the future projections of land conversion used in the IPCC may underestimate potential impacts of LULCC. By including a ‘business as usual’ future LULCC scenario for tropical deforestation, we find that even if all non-LULCC emissions are switched off in 2015, it is likely that 1.5 °C of warming relative to the preindustrial era will occur by 2100. Thus, policies to reduce LULCC emissions must remain a high priority if we are to achieve the low to medium temperature change targets proposed as a part of the Paris Agreement. Future studies using integrated assessment models and other climate simulations should include more realistic deforestation rates and the integration of policy that would reduce LULCC emissions.https://doi.org/10.1088/1748-9326/aa836dland useclimate changeagriculturedeforestation
spellingShingle Natalie M Mahowald
Daniel S Ward
Scott C Doney
Peter G Hess
James T Randerson
Are the impacts of land use on warming underestimated in climate policy?
Environmental Research Letters
land use
climate change
agriculture
deforestation
title Are the impacts of land use on warming underestimated in climate policy?
title_full Are the impacts of land use on warming underestimated in climate policy?
title_fullStr Are the impacts of land use on warming underestimated in climate policy?
title_full_unstemmed Are the impacts of land use on warming underestimated in climate policy?
title_short Are the impacts of land use on warming underestimated in climate policy?
title_sort are the impacts of land use on warming underestimated in climate policy
topic land use
climate change
agriculture
deforestation
url https://doi.org/10.1088/1748-9326/aa836d
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