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      Plants with less chlorophyll: A global change perspective

      1 , 2 , 1 , 3
      Global Change Biology
      Wiley

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          Abstract

          <p id="d1357142e222">The necessary reduction of greenhouse gas (GHG) emissions may lead in the future to an increase in solar irradiance (solar brightening). Anthropogenic aerosols (and their precursors) that cause solar dimming are in fact often co‐emitted with GHGs. While the reduction of GHG emissions is expected to slow down the ongoing increase in the greenhouse effect, an increased surface irradiance due to reduced atmospheric aerosol load might occur in the most populated areas of the earth. Increased irradiance may lead to air warming, favour the occurrence of heatwaves and increase the evaporative demand of the atmosphere. This is why effective and sustainable solar radiation management strategies to reflect more light back to space should be designed, tested and implemented together with GHG emission mitigation. Here we propose that new plants (crops, orchards and forests) with low‐chlorophyll (Chl) content may provide a realistic, sustainable and relatively simple solution to increase surface reflectance of large geographical areas via changes in surface albedo. This may finally offset all or part of the expected local solar brightening. While high‐Chl content provides substantial competitive advantages to plants growing in their natural environment, new plants with low‐Chl content may be successfully used in agriculture and silviculture and be as productive as the green wildtypes (or even more). The most appropriate strategies to obtain highly productive and highly reflective plants are discussed in this paper and their mitigation potential is examined together with the challenges associated with their introduction in agriculture. </p><p class="first" id="d1357142e226">Climate change mitigation policies aimed at the reduction of greenhouse gas (GHG) emissions might cause an increase in solar irradiance in the most populated areas of the planet (solar brightening). Anthropogenic aerosols causing solar dimming are co‐emitted with GHGs. New plants with low‐chlorophyll (Chl) content may offset such brightening. Their introduction increases surface reflectance (albedo) of large geographical areas, thus reducing the shortwave radiative forcing (RFSW). Additional benefits such as reducing transpiration and/or mitigating local effects of extreme temperatures may be obtained. Genome editing aims to create those new plants targeting both appropriate optical properties and enhanced productivity. <div class="boxed-text panel" id="gcb15470-blkfxd-0001"> <a class="named-anchor" id="gcb15470-blkfxd-0001"> <!-- named anchor --> </a> <div class="figure-container so-text-align-c"> <img alt="" class="figure" src="/document_file/55e7a32a-1f57-46f1-9cf0-c214c3aee91b/PubMedCentral/image/GCB-27-959-g004.jpg"/> </div> <div class="panel-content"/> </div> </p>

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          Most cited references75

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          The Community Earth System Model: A Framework for Collaborative Research

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            Temporary reduction in daily global CO2 emissions during the COVID-19 forced confinement

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              Changes in air quality during the lockdown in Barcelona (Spain) one month into the SARS-CoV-2 epidemic

              Lockdown measures came into force in Spain from March 14th, two weeks after the start of the SARS-CoV-2 epidemic, to reduce the epidemic curve. Our study aims to describe changes in air pollution levels during the lockdown measures in the city of Barcelona (NE Spain), by studying the time evolution of atmospheric pollutants recorded at the urban background and traffic air quality monitoring stations. After two weeks of lockdown, urban air pollution markedly decreased but with substantial differences among pollutants. The most significant reduction was estimated for BC and NO2 (−45 to −51%), pollutants mainly related to traffic emissions. A lower reduction was observed for PM10 (−28 to −31.0%). By contrast, O3 levels increased (+33 to +57% of the 8 h daily maxima), probably due to lower titration of O3 by NO and the decrease of NOx in a VOC-limited environment. Relevant differences in the meteorology of these two periods were also evidenced. The low reduction for PM10 is probably related to a significant regional contribution and the prevailing secondary origin of fine aerosols, but an in-depth evaluation has to be carried out to interpret this lower decrease. There is no defined trend for the low SO2 levels, probably due to the preferential reduction in emissions from the least polluting ships. A reduction of most pollutants to minimal concentrations are expected for the forthcoming weeks because of the more restrictive actions implemented for a total lockdown, which entered into force on March 30th. There are still open questions on why PM10 levels were much less reduced than BC and NO2 and on what is the proportion of the abatement of pollution directly related to the lockdown, without meteorological interferences.
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                Author and article information

                Contributors
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                Journal
                Global Change Biology
                Glob Change Biol
                Wiley
                1354-1013
                1365-2486
                December 13 2020
                Affiliations
                [1 ]Institute for Bioeconomy (IBE) National Research Council (CNR) Firenze Italy
                [2 ]Department of Biotechnology University of Verona Verona Italy
                [3 ]Accademia dei Georgofili Firenze Italy
                Article
                10.1111/gcb.15470
                6f51c434-cd39-4282-8535-a2022837353e
                © 2020

                http://creativecommons.org/licenses/by-nc-nd/4.0/

                http://doi.wiley.com/10.1002/tdm_license_1.1

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