{"id":2009,"date":"2021-04-14T18:00:00","date_gmt":"2021-04-14T21:00:00","guid":{"rendered":"https:\/\/www.ufrgs.br\/conexoesamazonicas\/?p=2009"},"modified":"2021-04-14T20:23:16","modified_gmt":"2021-04-14T23:23:16","slug":"o-que-as-projecoes-climaticas-nos-dizem-sobre-o-futuro-dos-recursos-hidricos-na-amazonia","status":"publish","type":"post","link":"https:\/\/www.ufrgs.br\/conexoesamazonicas\/en\/o-que-as-projecoes-climaticas-nos-dizem-sobre-o-futuro-dos-recursos-hidricos-na-amazonia\/","title":{"rendered":"What do the climate projections tell us about the water resources in the Amazon?"},"content":{"rendered":"<div data-elementor-type=\"wp-post\" data-elementor-id=\"2009\" class=\"elementor elementor-2009\" data-elementor-settings=\"[]\">\n\t\t\t\t\t\t<div class=\"elementor-inner\">\n\t\t\t\t\t\t\t<div class=\"elementor-section-wrap\">\n\t\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-3f6b7a4b elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"3f6b7a4b\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-32bccb1b\" data-id=\"32bccb1b\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-4d18a1a9 elementor-widget elementor-widget-heading\" data-id=\"4d18a1a9\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">What do the climate projections tell us about the water resources in the Amazon?<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-4c4eb72b elementor-widget elementor-widget-spacer\" data-id=\"4c4eb72b\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-75c027ba elementor-widget elementor-widget-spacer\" data-id=\"75c027ba\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-66a6885c elementor-widget elementor-widget-text-editor\" data-id=\"66a6885c\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"color: #aaaaaa;\">15 April 2021 | Duration of reading: 9 minutes<\/p><p style=\"color: #aaaaaa;\"><i>By Jo\u00e3o Paulo Br\u00eada<\/i><\/p><p class=\"has-drop-cap\">Climate change has been a prominent theme in recent decades. This issue has been linked to the process of indiscriminate industrial development and ended up raising many environmental movements around the world. Political and inflammatory demonstrations brought debates that often disassociate themselves from science. Even though there is important research on the subject, there are still doubts and misinterpretations that lead to shallow, incoherent and biased discussions.<\/p><p><span style=\"font-weight: 400;\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 To begin, it is important to understand that climate variability is a natural process. On a scale of decades, we are faced with climatic phenomena such as El Ni\u00f1o and La Ni\u00f1a, which are related to temperature anomalies in the Pacific Ocean and significantly change the rain regime not only in the Amazon region but in several places in Brazil and the world (<\/span><a href=\"https:\/\/oceanservice.noaa.gov\/facts\/ninonina.html\" target=\"_blank\" rel=\"noopener\">more information about El Nin\u00f5 and La Nin\u00e3<\/a><span style=\"font-weight: 400;\">). On a scale of centuries and millennia, there are major climatic changes such as the appearance of ice ages (the latter 20,000 years ago) and other less abrupt periods such as the \u201cLittle Ice Age\u201d between 1500 and 1800 d.c. For more information on paleoclimatology, see the texto by researcher Rafael Reis, which discusses the past climate in the Amazon region, published <\/span><a href=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/en\/registros-do-passado-e-conexoes-entre-os-andes-e-amazonia\/\" target=\"_blank\" rel=\"noopener\">read more<\/a><span style=\"font-weight: 400;\">\u00a0at Conex\u00f5es Amaz\u00f4nicas.<\/span><\/p><p><span style=\"font-weight: 400;\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 However, the mobilization of scientists and world leaders consolidated through the IPCC (<\/span><a href=\"https:\/\/www.ipcc.ch\/\" target=\"_blank\" rel=\"noopener\">Intergovernamental Panel on Climate Change<\/a><span style=\"font-weight: 400;\">) highlights the human influence on the world climate. This is an attempt to reduce the effects on something that, unlike the natural climate variability, we have a certain responsibility. In urban areas, effects on climate due to anthropic actions are easily noticed, as is the case of\u00a0<\/span><a href=\"https:\/\/www.thoughtco.com\/temperature-inversion-layers-1434435\" target=\"_blank\" rel=\"noopener\">thermal inversion<\/a><span style=\"font-weight: 400;\">\u00a0and temperature increase due to the reduction of green areas (<\/span><a href=\"https:\/\/www.nationalgeographic.org\/encyclopedia\/urban-heat-island\/\" target=\"_blank\" rel=\"noopener\">heat islands<\/a><span style=\"font-weight: 400;\">). On a global scale, the human effect on the climate comes down to consequences from\u00a0<\/span><a href=\"https:\/\/ipam.org.br\/glossario\/greenhouse-gases-ghg\/\" target=\"_blank\" rel=\"noopener\">greenhouse gases (GHG)<\/a><span style=\"font-weight: 400;\"> emissions to the atmosphere. However, this effect is not so noticeable because it consists of a complex process that is mixed with natural variations that occurs between years, seasons, and due to specific atmospheric phenomena. <\/span><\/p><p><span style=\"font-weight: 400;\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 An alternative to detect and project these impacts is to use current scientific knowledge in the development of <\/span><a href=\"https:\/\/www.wcrp-climate.org\/wgcm-cmip\" target=\"_blank\" rel=\"noopener\">climate models<\/a><span style=\"font-weight: 400;\">. Climate models are mathematical tools that represent, in the form of physical equations, the balance of mass and energy that occurs in the atmosphere, oceans, soil and glaciers. They are able to simulate approximately the current climate of the planet and make predictions using projected concentration of GHGs in the atmosphere as input data. These models then provide climate information such as: temperature, rain, air humidity, atmospheric pressure, among others.<\/span><\/p><p><span style=\"font-weight: 400;\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 To obtain more accurate estimates of the impact on water resources, we forced a hydrological model with output data from climate models.<\/span><span style=\"font-weight: 400;\">\u00a0With a similar concept, hydrological models use rainfall data as an input to simulate runoff, infiltration, evapotranspiration and soil moisture variation in river basins, and usually also estimate river flows. In the Figure 1 below we highlight the Amazon Basin, which is one of the study areas from our research about projections of climate change impacts on water resources related to the end of that century (2080-2100), a  work carried out within the Large Scale Hydrology research group, at the UFRGS Hydraulic Research Institute. (<\/span><a href=\"https:\/\/link.springer.com\/article\/10.1007\/s10584-020-02667-9\" target=\"_blank\" rel=\"noopener\">Research link<\/a><span style=\"font-weight: 400;\">).<\/span><\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-34af2c1e elementor-widget elementor-widget-image\" data-id=\"34af2c1e\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image\">\n\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img width=\"887\" height=\"600\" src=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1.png\" class=\"attachment-2048x2048 size-2048x2048\" alt=\"\" loading=\"lazy\" srcset=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1.png 568w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1-300x208.png 300w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1-16x12.png 16w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1-230x160.png 230w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1-350x243.png 350w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem1-1-480x333.png 480w\" sizes=\"(max-width: 887px) 100vw, 887px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\"><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-545f9cdf elementor-widget elementor-widget-text-editor\" data-id=\"545f9cdf\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Figure 1. Main Hydrographic Basins in the Amazon region and their location in South America.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-205a9baa elementor-widget elementor-widget-text-editor\" data-id=\"205a9baa\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p>\u00a0 \u00a0 \u00a0 \u00a0 <span style=\"font-weight: 400;\">In this study, we used data from 25 global climate models in order to assess the uncertainties of the climate projections. The analysis is related to the scenario\u00a0<\/span><a href=\"https:\/\/sos.noaa.gov\/datasets\/climate-model-temperature-change-rcp-45-2006-2100\/\" target=\"_blank\" rel=\"noopener\">RCP4.5<\/a><span style=\"font-weight: 400;\">\u00a0, which is one of the most used scenarios and represents a future with industrial development and GHG emissions under reasonable control.<\/span><\/p><p>\u00a0 \u00a0 \u00a0 \u00a0 <span style=\"font-weight: 400;\">Our results showed a considerable increase in the average annual temperature (between 2 and 3 <\/span><span style=\"font-weight: 400;\">o<\/span><span style=\"font-weight: 400;\">C), throughout the Amazon region, and a little lower in the western extreme of the basin, as we can see in Figure 2. These results do not imply that some harsh winters and mild summers will cease to exist, as these are part of the natural variability, but maybe they will be less frequent. It is also observed that there will be a reduction in precipitation between 5 and 20% mainly in the eastern part of the basin and an increase in the extreme west (5 to 20% in the Andean region). Evaporation, on the other hand, will increase practically throughout the Amazon region, probably due to the expected increase in temperature and the large availability of water in the basin.<\/span><\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-55874425 elementor-widget elementor-widget-image\" data-id=\"55874425\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image\">\n\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img width=\"567\" height=\"203\" src=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1.png\" class=\"attachment-large size-large\" alt=\"\" loading=\"lazy\" srcset=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1.png 567w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1-300x111.png 300w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1-16x6.png 16w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1-230x85.png 230w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1-350x130.png 350w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem2-1-480x178.png 480w\" sizes=\"(max-width: 567px) 100vw, 567px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\"><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-6b487cb8 elementor-widget elementor-widget-text-editor\" data-id=\"6b487cb8\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Figure 2. Change of Temperature, Precipitation and Evapotranspiration projected for the end of this century compared to nowadays.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-165d198 elementor-widget elementor-widget-text-editor\" data-id=\"165d198\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p>\u00a0 \u00a0 \u00a0 \u00a0 <span style=\"font-weight: 400;\">The increase in evaporation combined with the decrease in precipitation causes a great reduction in streamflow, mainly in the eastern part of the basin. The runoff reductions are presented in Figure 3.<\/span><\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5ac840cf elementor-widget elementor-widget-image\" data-id=\"5ac840cf\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image\">\n\t\t\t\t\t\t\t\t\t\t<img width=\"1024\" height=\"514\" src=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1.png\" class=\"attachment-large size-large\" alt=\"\" loading=\"lazy\" srcset=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1.png 600w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1-300x156.png 300w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1-16x8.png 16w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1-230x119.png 230w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1-350x181.png 350w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/Imagem3-1-480x249.png 480w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-2f8df0f0 elementor-widget elementor-widget-spacer\" data-id=\"2f8df0f0\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1b81b61 elementor-widget elementor-widget-text-editor\" data-id=\"1b81b61\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Figure 3. a) Map of the relative change of runoff projected for the end of the century compared to current days in the Amazon region. b) Hydrographs of some important basins in the Amazon. Black Line is the current discharge regime and the grey swath represents the inter-quartile distance related to the 25 climate models ensemble.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-653d430c elementor-widget elementor-widget-spacer\" data-id=\"653d430c\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1b0fc213 elementor-widget elementor-widget-text-editor\" data-id=\"1b0fc213\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p>\u00a0 \u00a0 \u00a0 \u00a0 <span style=\"font-weight: 400;\">There is a great tendency to decrease the runoff, mainly in the eastern part of the Amazon basin, where the Xingu and Tapaj\u00f3s rivers are. We can see how the current streamflow (black line in the figure above) is well above the range of projections (in gray) generated by the hydrological model fed with climate data. This implies reductions of 10 to 20% in the waters flowing at the rivers Madeira, Amazon, Purus and even more than 30% of reduction in the Xingu and Tapaj\u00f3s rivers.<\/span><\/p><p><span style=\"font-weight: 400;\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 The results achieved in this study provide valuable information for the planning and management of natural resources. Given the current conditions of development, it is inevitable that engineering projects and resource planning consider information from climate projections. Otherwise, unwanted climatic effects will be common and may even have their impacts amplified.<\/span><\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-45e21e28 elementor-widget elementor-widget-text-editor\" data-id=\"45e21e28\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p><strong>\u00a0<\/strong><strong>Science is done collaboratively<\/strong><\/p><p>\u00a0 \u00a0 \u00a0 \u00a0 <span style=\"font-weight: 400;\">This study was conducted by the Large Scale Hydrology research group, at the Hydraulic Research Institute of UFRGS. This work belongs to a project in partnership with INPE (Instituto Nacional de Pesquisas Espaciais) and financed by CAPES and ANA (Brazilian National Water Agency).<\/span><\/p><p><strong>Want to know more? Access the links below!<\/strong><\/p><p>Br\u00eada, Jo\u00e3o Paulo Lyra Fialho, et al. &#8220;Climate change impacts on South American water balance from a continental-scale hydrological model driven by CMIP5 projections.&#8221; Climatic Change 159.4 (2020): 503-522. (<a href=\"https:\/\/link.springer.com\/article\/10.1007\/s10584-020-02667-9\" target=\"_blank\" rel=\"noopener\">Access here<\/a>)<\/p><p>IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stoker, T.F., Qin, G-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. (<a href=\"https:\/\/www.ipcc.ch\/site\/assets\/uploads\/2018\/02\/WG1AR5_SPM_FINAL.pdf\" target=\"_blank\" rel=\"noopener\">Access here<\/a>)<\/p><p>Global Climate Change. Vital Signs of the Planet. (<a href=\"https:\/\/climate.nasa.gov\/\" target=\"_blank\" rel=\"noopener\">climate.nasa.gov<\/a>)<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1c7d7d49 elementor-widget elementor-widget-image\" data-id=\"1c7d7d49\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image\">\n\t\t\t\t\t\t\t\t\t\t<img width=\"263\" height=\"300\" src=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1-263x300.jpg\" class=\"attachment-medium size-medium\" alt=\"\" loading=\"lazy\" srcset=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1-263x300.jpg 263w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1-11x12.jpg 11w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1-230x263.jpg 230w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1-350x400.jpg 350w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1-480x549.jpg 480w, https:\/\/www.ufrgs.br\/conexoesamazonicas\/wp-content\/uploads\/2021\/04\/WIN_20210322_14_22_33_Pro2-1.jpg 630w\" sizes=\"(max-width: 263px) 100vw, 263px\" \/>\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-7876b735 elementor-widget elementor-widget-text-editor\" data-id=\"7876b735\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Jo\u00e3o Paulo Br\u00eada - Sanitary and Environmental Engineer of the Alagoas Federal University (UFAL). Master degree and current PhD student of Water Resourses and Environmental Sanitation at the Hydraulic Researchs Institute (IPH) of the Rio Grande do Sul Federal University (UFRGS).<\/p>\n<p style=\"text-align: center;\">More information on&nbsp;<a href=\"http:\/\/buscatextual.cnpq.br\/buscatextual\/visualizacv.do?id=K4477308Z5\" target=\"_blank\" rel=\"noopener\">Lattes Platform<\/a>&nbsp;or contact by&nbsp;<a href=\"mailto:joaopaulolfb@gmail.com\" target=\"_blank\">e-mail<\/a>.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>15 April 2021 by Jo\u00e3o Paulo Br\u00eada<\/p>","protected":false},"author":1,"featured_media":2019,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0},"categories":[7],"tags":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v15.7 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>O que as proje\u00e7\u00f5es clim\u00e1ticas nos dizem sobre o futuro dos recursos h\u00eddricos na Amaz\u00f4nia? 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