{"id":288416,"date":"2019-06-18T16:52:04","date_gmt":"2019-06-18T19:52:04","guid":{"rendered":"http:\/\/revistapesquisa.fapesp.br\/?p=288416"},"modified":"2019-06-18T17:32:43","modified_gmt":"2019-06-18T20:32:43","slug":"hotter-and-drier-cities","status":"publish","type":"post","link":"https:\/\/revistapesquisa.fapesp.br\/en\/hotter-and-drier-cities\/","title":{"rendered":"Hotter and drier cities"},"content":{"rendered":"<p>In the worst-case scenario as modeled in the most recent Intergovernmental Panel on Climate Change (IPCC) report, greenhouse gas emissions would continue to increase through the end of the century, and average atmospheric temperatures would warm by around 4 \u00b0C from current temperatures. If these global climate predictions materialize in the coming decades, maximum summer temperatures could rise by up to 9 \u00baC and rainfall would be halved in Brazil\u2019s two largest metropolitan areas\u2014S\u00e3o Paulo and Rio de Janeiro\u2014and in Santos, home to Brazil\u2019s most important port. Minimum temperatures in these areas can also be expected to rise by about 4 \u00b0C by the end of the century, meaning winters would also be warmer.<\/p>\n<p>These projections for parts of Brazil\u2019s Southeast are from a paper published by researchers from the Brazilian National Institute for Space Research (INPE), the Federal University of Rio de Janeiro (UFRJ), and the Center for Natural Disasters Monitoring (CEMADEN) in the April issue of <em>Theoretical and Applied Climatology<\/em>. \u201cIf the current greenhouse gas emissions trends continue, the probability of the study data materializing will likely be high,\u201d says meteorologist Andr\u00e9 Lyra, a postdoctoral fellow at INPE and the study\u2019s lead author.<\/p>\n<p>The Brazilian team modeled potential temperatures and rainfall rates in the three metropolitan areas assuming two of the IPCC\u2019s global climate scenarios: the worst-case scenario, technically designated as RCP8.5, and the best-case scenario, RCP4.5. In the second scenario, greenhouse gas emissions would stop rising in the 2040s. However, even when this less alarming projection is assumed in the Eta Regional Climate Model, which was partly developed by INPE, the modeling results are not substantially different. Maximum temperatures in S\u00e3o Paulo, Rio de Janeiro, and Santos rise by as much as 7 \u00baC and rainfall is reduced by half, although the lower rainfall rates affect a smaller portion of the metropolitan areas. While these scenarios carry some degree of uncertainty, they indicate that relatively intense climate change is likely.<\/p>\n<p>The researchers used an enhanced version of Eta with a spatial resolution of 25 square kilometers (km<sup>2<\/sup>), or a square with 5 km sides. The previous version had a resolution of 400 km<sup>2<\/sup> (a square with 20 km sides). \u201cThe new model is important for an understanding of climate-change impacts on certain aspects of South American topography,\u201d says meteorologist Chou Sin Chan of INPE, who coauthored the paper. \u201cA study with 5 km resolution provides a higher level of detail than a study with 20 km resolution.\u201d In this version of Eta there are fewer calculation errors for climate predictions in areas with rugged terrain. This enhancement has important implications when investigating locations near mountainous areas, such as Serra do Mar and Mantiqueira, two mountain ranges in the vicinity of the study area.<\/p>\n<p>Climate projections in the three metropolitan areas were compared with historical data within the model from 1961 to 1990. The projections were divided into three slices, 2011\u20132040, 2041\u20132070, and 2071\u20132100. In addition to a general trend of warming and lower rainfall, the paper predicts extreme events such as extended droughts and severe storms will increase in intensity. In the Metropolitan Area of S\u00e3o Paulo, for example, the number of days of heat waves could increase by 60 days and the number of cold-wave days could decrease by three days at around 2100. The study also predicts that days and nights will become more uncomfortable in the three study areas, placing an increased demand on cooling equipment and consequently increasing energy consumption. This could also create potential health risks for the poor and elderly.<\/p>\n<p>\u201cExtremes have a bigger effect on our lives,\u201d says Claudine Dereczynski, a meteorologist at the Federal University of Rio de Janeiro (UFRJ) and a coauthor of the paper. \u201cThe increasing occurrence of events of this kind is a greater concern stemming from climate change than changes in average precipitation or temperature.\u201d The model also predicts that extremely heavy rainfall events will intensify toward the end of the twenty-first century, causing frequent landslides. Dereczynski notes that the projections are more reliable for changes in temperature than in rainfall.<\/p>\n<p>The study underscores how the high population density in the metropolitan areas of Rio and S\u00e3o Paulo, where 33 million people live, has led to improper land use and severe degradation of natural resources. \u201cClimate-change research depends heavily on acceptance by different industries, and public awareness, of the importance of taking action to mitigate the effects of greenhouse gas emissions,\u201d says sociologist Pedro Roberto Jacobi, a professor at the Institute for Energy and the Environment at the University of S\u00e3o Paulo (IEE-USP). \u201cOur research shows that municipal governments could even implement decarbonization initiatives on a local scale, such as erosion control through changes in land-use legislation or improved solid waste management policy. But global action is needed\u2014which depends on agreements between nations\u2014to mitigate climate change.\u201d<\/p>\n<p class=\"bibliografia separador-bibliografia\"><strong>Project<\/strong><br \/>\nAn integrated framework to analyze local capacity for decision-making and adaptation to large-scale environmental change: Community case studies in Brazil, the UK, and the US (<a href=\"https:\/\/bv.fapesp.br\/pt\/auxilios\/81993\/uma-estrutura-integrada-para-analisar-tomada-de-decisao-local-e-capacidade-adaptativa-para-mudanca-a\/?q=12\/51876-0\" target=\"_blank\" rel=\"noopener noreferrer\">no. 12\/51876-0<\/a>); <strong>Grant Mechanism<\/strong> Thematic Project; FAPESP-Belmont Forum Agreement; <strong>Principal Investigator<\/strong> Jos\u00e9 Marengo (CEMADEN); <strong>Investment<\/strong> R$711,506.53.<\/p>\n<p class=\"bibliografia\"><strong>Scientific article<\/strong><br \/>\nLYRA, A. <em>et al<\/em>. <a href=\"https:\/\/link.springer.com\/article\/10.1007\/s00704-017-2067-z\" target=\"_blank\" rel=\"noopener noreferrer\">Climate change projections over three metropolitan regions in Southeast Brazil using the non-hydrostatic Eta regional climate model at 5-km resolution<\/a>.\u00a0<strong>Theoretical and Applied Climatology<\/strong>. Vol. 132, no. 1-2, pp. 663\u201382. Apr. 2018.<\/p>\n","protected":false},"excerpt":{"rendered":"Modeling indicates temperatures will rise and rainfall will be halved in S\u00e3o Paulo, Rio de Janeiro, and Santos by the end of the century","protected":false},"author":665,"featured_media":288417,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_exactmetrics_skip_tracking":false,"_exactmetrics_sitenote_active":false,"_exactmetrics_sitenote_note":"","_exactmetrics_sitenote_category":0,"footnotes":""},"categories":[166],"tags":[200],"coauthors":[2174],"class_list":["post-288416","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-policies-st-en","tag-environment"],"acf":[],"_links":{"self":[{"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/posts\/288416","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/users\/665"}],"replies":[{"embeddable":true,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/comments?post=288416"}],"version-history":[{"count":5,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/posts\/288416\/revisions"}],"predecessor-version":[{"id":292311,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/posts\/288416\/revisions\/292311"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/media\/288417"}],"wp:attachment":[{"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/media?parent=288416"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/categories?post=288416"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/tags?post=288416"},{"taxonomy":"author","embeddable":true,"href":"https:\/\/revistapesquisa.fapesp.br\/en\/wp-json\/wp\/v2\/coauthors?post=288416"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}