E. Davin, D. Rechid, M. Breil, R. Cardoso, E. Coppola, P. Hoffmann, L. Jach, E. Katragkou, N. de Noblet‐Ducoudré, K. Radtke, M. Raffa, P. Soares, Giannis Sofiadis, S. Strada, G. Strandberg, M. Tölle, K. Warrach‐Sagi, V. Wulfmeyer
{"title":"欧洲造林的生物地球物理影响:来自LUCAS(土地利用和跨尺度气候)区域气候模式相互比较的初步结果","authors":"E. Davin, D. Rechid, M. Breil, R. Cardoso, E. Coppola, P. Hoffmann, L. Jach, E. Katragkou, N. de Noblet‐Ducoudré, K. Radtke, M. Raffa, P. Soares, Giannis Sofiadis, S. Strada, G. Strandberg, M. Tölle, K. Warrach‐Sagi, V. Wulfmeyer","doi":"10.5194/esd-11-183-2020","DOIUrl":null,"url":null,"abstract":"Abstract. The Land Use and Climate Across Scales Flagship Pilot\nStudy (LUCAS FPS) is a coordinated community effort to improve the\nintegration of land use change (LUC) in regional climate models (RCMs) and\nto quantify the biogeophysical effects of LUC on local to regional climate\nin Europe. In the first phase of LUCAS, nine RCMs are used to explore the\nbiogeophysical impacts of re-/afforestation over Europe: two\nidealized experiments representing respectively a non-forested and a\nmaximally forested Europe are compared in order to quantify spatial and\ntemporal variations in the regional climate sensitivity to forestation. We\nfind some robust features in the simulated response to forestation. In\nparticular, all models indicate a year-round decrease in surface albedo,\nwhich is most pronounced in winter and spring at high latitudes. This\nresults in a winter warming effect, with values ranging from +0.2 to +1 \nK on average over Scandinavia depending on models. However, there are also a\nnumber of strongly diverging responses. For instance, there is no agreement\non the sign of temperature changes in summer with some RCMs predicting a\nwidespread cooling from forestation (well below −2 K in most regions), a\nwidespread warming (around +2 K or above in most regions) or a mixed\nresponse. A large part of the inter-model spread is attributed to the\nrepresentation of land processes. In particular, differences in the\npartitioning of sensible and latent heat are identified as a key source of\nuncertainty in summer. Atmospheric processes, such as changes in incoming\nradiation due to cloud cover feedbacks, also influence the simulated\nresponse in most seasons. In conclusion, the multi-model approach we use\nhere has the potential to deliver more robust and reliable information to\nstakeholders involved in land use planning, as compared to results based on\nsingle models. However, given the contradictory responses identified, our\nresults also show that there are still fundamental uncertainties that need\nto be tackled to better anticipate the possible intended or unintended\nconsequences of LUC on regional climates.","PeriodicalId":11466,"journal":{"name":"Earth System Dynamics Discussions","volume":"69 1","pages":"183-200"},"PeriodicalIF":0.0000,"publicationDate":"2020-02-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"59","resultStr":"{\"title\":\"Biogeophysical impacts of forestation in Europe: first results from the LUCAS (Land Use and Climate Across Scales) regional climate model intercomparison\",\"authors\":\"E. Davin, D. Rechid, M. Breil, R. Cardoso, E. Coppola, P. Hoffmann, L. Jach, E. Katragkou, N. de Noblet‐Ducoudré, K. Radtke, M. Raffa, P. Soares, Giannis Sofiadis, S. Strada, G. Strandberg, M. Tölle, K. Warrach‐Sagi, V. Wulfmeyer\",\"doi\":\"10.5194/esd-11-183-2020\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. The Land Use and Climate Across Scales Flagship Pilot\\nStudy (LUCAS FPS) is a coordinated community effort to improve the\\nintegration of land use change (LUC) in regional climate models (RCMs) and\\nto quantify the biogeophysical effects of LUC on local to regional climate\\nin Europe. In the first phase of LUCAS, nine RCMs are used to explore the\\nbiogeophysical impacts of re-/afforestation over Europe: two\\nidealized experiments representing respectively a non-forested and a\\nmaximally forested Europe are compared in order to quantify spatial and\\ntemporal variations in the regional climate sensitivity to forestation. We\\nfind some robust features in the simulated response to forestation. In\\nparticular, all models indicate a year-round decrease in surface albedo,\\nwhich is most pronounced in winter and spring at high latitudes. This\\nresults in a winter warming effect, with values ranging from +0.2 to +1 \\nK on average over Scandinavia depending on models. However, there are also a\\nnumber of strongly diverging responses. For instance, there is no agreement\\non the sign of temperature changes in summer with some RCMs predicting a\\nwidespread cooling from forestation (well below −2 K in most regions), a\\nwidespread warming (around +2 K or above in most regions) or a mixed\\nresponse. A large part of the inter-model spread is attributed to the\\nrepresentation of land processes. In particular, differences in the\\npartitioning of sensible and latent heat are identified as a key source of\\nuncertainty in summer. Atmospheric processes, such as changes in incoming\\nradiation due to cloud cover feedbacks, also influence the simulated\\nresponse in most seasons. In conclusion, the multi-model approach we use\\nhere has the potential to deliver more robust and reliable information to\\nstakeholders involved in land use planning, as compared to results based on\\nsingle models. However, given the contradictory responses identified, our\\nresults also show that there are still fundamental uncertainties that need\\nto be tackled to better anticipate the possible intended or unintended\\nconsequences of LUC on regional climates.\",\"PeriodicalId\":11466,\"journal\":{\"name\":\"Earth System Dynamics Discussions\",\"volume\":\"69 1\",\"pages\":\"183-200\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-02-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"59\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earth System Dynamics Discussions\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5194/esd-11-183-2020\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth System Dynamics Discussions","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/esd-11-183-2020","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Biogeophysical impacts of forestation in Europe: first results from the LUCAS (Land Use and Climate Across Scales) regional climate model intercomparison
Abstract. The Land Use and Climate Across Scales Flagship Pilot
Study (LUCAS FPS) is a coordinated community effort to improve the
integration of land use change (LUC) in regional climate models (RCMs) and
to quantify the biogeophysical effects of LUC on local to regional climate
in Europe. In the first phase of LUCAS, nine RCMs are used to explore the
biogeophysical impacts of re-/afforestation over Europe: two
idealized experiments representing respectively a non-forested and a
maximally forested Europe are compared in order to quantify spatial and
temporal variations in the regional climate sensitivity to forestation. We
find some robust features in the simulated response to forestation. In
particular, all models indicate a year-round decrease in surface albedo,
which is most pronounced in winter and spring at high latitudes. This
results in a winter warming effect, with values ranging from +0.2 to +1
K on average over Scandinavia depending on models. However, there are also a
number of strongly diverging responses. For instance, there is no agreement
on the sign of temperature changes in summer with some RCMs predicting a
widespread cooling from forestation (well below −2 K in most regions), a
widespread warming (around +2 K or above in most regions) or a mixed
response. A large part of the inter-model spread is attributed to the
representation of land processes. In particular, differences in the
partitioning of sensible and latent heat are identified as a key source of
uncertainty in summer. Atmospheric processes, such as changes in incoming
radiation due to cloud cover feedbacks, also influence the simulated
response in most seasons. In conclusion, the multi-model approach we use
here has the potential to deliver more robust and reliable information to
stakeholders involved in land use planning, as compared to results based on
single models. However, given the contradictory responses identified, our
results also show that there are still fundamental uncertainties that need
to be tackled to better anticipate the possible intended or unintended
consequences of LUC on regional climates.