{"id":14488,"date":"2021-02-04T15:00:06","date_gmt":"2021-02-04T15:00:06","guid":{"rendered":"https:\/\/conexoesamazonicas.org\/?post_type=artigos&#038;p=14488"},"modified":"2025-06-16T02:46:18","modified_gmt":"2025-06-16T02:46:18","slug":"vamos-quantificar-o-ciclo-da-agua2","status":"publish","type":"post","link":"https:\/\/conexoesamazonicas.org\/en\/vamos-quantificar-o-ciclo-da-agua2\/","title":{"rendered":"How to quantify the water cycle?"},"content":{"rendered":"<div data-elementor-type=\"wp-post\" data-elementor-id=\"14488\" class=\"elementor elementor-14488\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-42cc7e2a elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"42cc7e2a\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-6acf3502\" data-id=\"6acf3502\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-a45989f elementor-widget elementor-widget-heading\" data-id=\"a45989f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">How to quantify the water cycle?<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-575b13d5 elementor-widget elementor-widget-spacer\" data-id=\"575b13d5\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-6a78fedd elementor-widget elementor-widget-spacer\" data-id=\"6a78fedd\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-587f834b elementor-widget elementor-widget-text-editor\" data-id=\"587f834b\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p style=\"color: #aaaaaa;\">4 February 2021 | Duration of reading: 8 min<\/p><p style=\"color: #aaaaaa;\"><i>By Adriana Moreira<\/i><\/p><p class=\"has-drop-cap\">We know that the Amazon tropical forest has huge importance to regional and global climate. But why is the Amazon forest so important for this? So, the Amazon forest vegetation exerts an incredible work recycling the water from the surface to the atmosphere, through the so-called evapotranspiration process. In addition, the forest also exerts a crucial role in the other water cycle processes (also known as hydrological processes), such as water soil infiltration. Understanding these hydrological processes allows us to improve our knowledge about important questions. For instance, what happens if we remove part of forest vegetation cover in a region such as the Amazon? How can deforestation affect the water exchange or the river discharge?<\/p><p>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 When we realize how huge the\u00a0<a href=\"https:\/\/www.amazoniacienciaciudadana.org\/portugues\/novidades\/rios-conectados\/\" target=\"_blank\" rel=\"noopener\">Amazon Basin<\/a>is, we often ask ourselves if it would be possible to monitor and measure all water cycle variables across the basin, especially for a long-term period. For instance, how much does it rain per day in each square kilometer in the Amazon basin? One way to answer this question is to use field measurements from the\u00a0<a href=\"http:\/\/www.snirh.gov.br\/hidroweb\/apresentacao\" target=\"_blank\" rel=\"noopener\">Brazilian Water and Sanitation Agency (ANA)<\/a>, which provides rainfall, runoff, and measurements of water levels for several rivers in Brazil. In addition, a range of satellites monitors the Earth\u2019s surface, estimates water cycle variables with significant accuracy, covering remote regions where field measurements are often unable to cover. Satellite data have been increasingly important for hydrological studies, providing information on water availability and impacts of land use and cover changes on the water cycle. If you want to know more about this subject, check the recent text by Leonardo Laipelt on the Conex\u00f5es Amaz\u00f4nicas Blog (<a href=\"https:\/\/www.ufrgs.br\/conexoesamazonicas\/utilizando-imagens-de-satelites-para-estimar-evapotranspiracao\/\" target=\"_blank\" rel=\"noopener\">see here<\/a>), and learn more about evapotranspiration estimation based on satellite images, and how this can help us understanding impacts on the water cycle caused by human activity.<\/p><p>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 In our article \u201c\u00a0<a href=\"https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0022169419304664\" target=\"_blank\" rel=\"noopener\">Assessment of terrestrial water balance using remote sensing data in South America<\/a>\u201d we investigated the Amazon water cycle through a water balance approach. But what is\u00a0<a href=\"https:\/\/pt.wikipedia.org\/wiki\/Balan%C3%A7o_h%C3%ADdrico\" target=\"_blank\" rel=\"noopener\">water balance<\/a>? Balan\u00e7o h\u00eddrico \u00e9 um m\u00e9todo onde contabilizamos as sa\u00eddas e entradas de \u00e1gua em um sistema \u2013 no nosso estudo, os sistemas s\u00e3o as bacias hidrogr\u00e1ficas \u2013 por um determinado per\u00edodo (semanas, meses, anos). Por exemplo, na figura abaixo temos uma ilustra\u00e7\u00e3o das sa\u00eddas e entradas de fluxos de \u00e1gua\u00a0 representadas por setas, onde podemos quantificar o volume de \u00e1gua que entrou no sistema por meio da precipita\u00e7\u00e3o (chuva) e o que saiu pelo escoamento dos rios (vaz\u00e3o) e evapotranspira\u00e7\u00e3o da vegeta\u00e7\u00e3o e dos solos. A diferen\u00e7a entre esses fluxos que entram e saem do sistema corresponde \u00e0 varia\u00e7\u00e3o do armazenamento de \u00e1gua.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-23f90c9 elementor-widget elementor-widget-spacer\" data-id=\"23f90c9\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-3531421f elementor-widget elementor-widget-image\" data-id=\"3531421f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"1280\" height=\"720\" src=\"https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/ATTO2.jpg\" class=\"attachment-1536x1536 size-1536x1536 wp-image-1127\" alt=\"\" srcset=\"https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/ATTO2.jpg 1280w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/ATTO2-300x169.jpg 300w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/ATTO2-1024x576.jpg 1024w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/ATTO2-768x432.jpg 768w\" sizes=\"(max-width: 1280px) 100vw, 1280px\" \/>\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\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5e06f916 elementor-widget elementor-widget-text-editor\" data-id=\"5e06f916\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p style=\"text-align: center;\">Water balance representation. The arrows indicate water inputs, through precipitation, and outputs, through river discharges and evapotranspiration, in the system. Figure adapted from the photo by Jorge Saturno (MPI-C), from the tower from\u00a0<span style=\"color: var( --e-global-color-text );\">Jorge Saturno (MPI-C) from\u00a0<\/span><span style=\"color: var( --e-global-color-text );\">torre do\u00a0<\/span><a href=\"https:\/\/www.attoproject.org\/pt\/\" target=\"_blank\" rel=\"noopener\">ATTO tower<\/a><span style=\"color: var( --e-global-color-text );\">.<\/span><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-7079349 elementor-widget elementor-widget-spacer\" data-id=\"7079349\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5ceac152 elementor-widget elementor-widget-text-editor\" data-id=\"5ceac152\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 How can we estimate the water cycle variables for a basin, at long-term periods? As we mentioned before, many of these hydrological variables can be estimated by satellite data. In this study we used evapotranspiration data from two different sources,\u00a0<a href=\"https:\/\/www.gleam.eu\/\" target=\"_blank\" rel=\"noopener\">GLEAM\u00a0<\/a>and\u00a0<a href=\"https:\/\/modis.gsfc.nasa.gov\/data\/dataprod\/mod16.php\" target=\"_blank\" rel=\"noopener\">MOD16<\/a>, precipitation data from\u00a0<a href=\"https:\/\/gpm.nasa.gov\/missions\/trmm\" target=\"_blank\" rel=\"noopener\">TRMM\u00a0<\/a>and\u00a0<a href=\"http:\/\/www.gloh2o.org\/\" target=\"_blank\" rel=\"noopener\">MSWEP<\/a>, data from the\u00a0<a href=\"https:\/\/pt.wikipedia.org\/wiki\/Gravity_Recovery_and_Climate_Experiment\" target=\"_blank\" rel=\"noopener\">GRACE\u00a0<\/a>mission to obtain terrestrial water storage changes, and field measurements of river discharges from<a href=\"http:\/\/www.snirh.gov.br\/hidroweb\/apresentacao\" target=\"_blank\" rel=\"noopener\">ANA<\/a>. We opted to use more than one source of data, for both precipitation and evapotranspiration because we know these satellite estimations have certain uncertainties. By using more than one source we could evaluate these datasets to verify which of them provide results with a better accuracy.<\/p><p>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 Based on the water balance approach we can estimate variables that are still hard to measure in the field or those which do not have high-density cover, such as river discharges. For instance, in our study, we computed the river discharges using only satellite data based on the water balance approach and compared the results with field river discharge measurements from ANA. Then we assessed the uncertainty of the satellite estimates. In the figure below we can see the uncertainty for river discharges indicated by the shaded area, for three large Amazonian river basins (Amazon, Tapaj\u00f3s, and Tocantins Rivers). In addition, we can also verify that the estimated river discharges based on satellite data (black line) are very close to ANA measurements (red line). Therefore, we were able to show that it is possible to estimate river discharges through the water balance, and the uncertainty associated with it.\u00a0<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-42a52e56 elementor-widget elementor-widget-image\" data-id=\"42a52e56\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"1024\" height=\"724\" src=\"https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-1024x724.jpg\" class=\"attachment-large size-large wp-image-1132\" alt=\"\" srcset=\"https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-1024x724.jpg 1024w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-300x212.jpg 300w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-768x543.jpg 768w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-1536x1086.jpg 1536w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-2048x1448.jpg 2048w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/Sazonalidade-vazao-scaled-1-1568x1109.jpg 1568w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\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\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1c65ff4d elementor-widget elementor-widget-text-editor\" data-id=\"1c65ff4d\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p style=\"text-align: center;\">Estimation of river discharge\u2019 seasonality with the water balance approach using satellite data (black line), and measured by the Brazilian Water Agency (ANA) (red line), for the Amazon, Tapaj\u00f3s, and Tocantins basins. Shadow area represents the uncertainty of runoff estimates.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-48d713e1 elementor-widget elementor-widget-spacer\" data-id=\"48d713e1\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-21e37af6 elementor-widget elementor-widget-spacer\" data-id=\"21e37af6\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-3e5c31a2 elementor-widget elementor-widget-text-editor\" data-id=\"3e5c31a2\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>&nbsp; &nbsp; &nbsp; &nbsp; &nbsp; Based on the water balance approach we can also improve our knowledge about how the precipitation and evapotranspiration regimes vary, providing information about past flood and drought events. However, this will be the subject of a next text!&nbsp;<\/p><p>&nbsp;&nbsp; &nbsp; &nbsp; &nbsp; &nbsp;It is essential that we understand the water cycle and develop methods to quantify its components. Studies such as the one presented here have reinforced the great potential of using satellite data to monitor, evaluate and quantify water cycle dynamics.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-7c9c665 elementor-widget elementor-widget-spacer\" data-id=\"7c9c665\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\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\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-9d2823 elementor-widget elementor-widget-text-editor\" data-id=\"9d2823\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>Science is done collaboratively<\/strong><\/p><p>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 This study is part of the doctoral research carried out by Adriana Moreira, through the graduate program in Water Resources and Environmental Sanitation at the Hydraulic Research Institute (IPH \/ UFRGS), under the guidance of Professor\u00a0<a href=\"https:\/\/www.ufrgs.br\/hge\/equipe\/professores\/ruhoff\/\" target=\"_blank\" rel=\"noopener\">Anderson Ruhoff<\/a>. This research had financial support from the National Council for Scientific and Technological Development (CNPq), in partnership with the Coordination for the Improvement of Higher Education Personnel (CAPES) and with the Brazilian Water Agency (ANA).<\/p><p><strong>Want to know more? Access the links below!\u00a0<\/strong><\/p><p>Builes-Jaramillo e Poveda (2018). Conjoint Analysis of Surface and Atmospheric Water Balances in the Andes-Amazon System. Water Resources Research. (<a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/full\/10.1029\/2017WR021338\" target=\"_blank\" rel=\"noopener\">Link<\/a>)<\/p><p>Maeda et al. (2017). Evapotranspiration seasonality across the Amazon Basin. Earth System Dynamics. (<a href=\"https:\/\/esd.copernicus.org\/articles\/8\/439\/2017\/\" target=\"_blank\" rel=\"noopener\">Link<\/a>)<\/p><p>Moreira et al. (2019). Assessment of terrestrial water balance using remote sensing data in South America. Journal of Hydrology. (<a href=\"https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0022169419304664\" target=\"_blank\" rel=\"noopener\">Link<\/a>)<\/p><p>Rodell et al. (2011). Estimating evapotranspiration using an observation based terrestrial water budget. Hydrological Processes. (<a href=\"https:\/\/onlinelibrary.wiley.com\/doi\/abs\/10.1002\/hyp.8369\" target=\"_blank\" rel=\"noopener\">Link<\/a>)<\/p><p>Swann e Koven (2017). A Direct Estimate of the Seasonal Cycle of Evapotranspiration over the Amazon Basin. Journal of Hydrometeorology. (<a href=\"https:\/\/journals.ametsoc.org\/view\/journals\/hydr\/18\/8\/jhm-d-17-0004_1.xml\" target=\"_blank\" rel=\"noopener\">Link<\/a>)<\/p><div>\u00a0<\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-746a6955 elementor-widget elementor-widget-image\" data-id=\"746a6955\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"300\" height=\"300\" src=\"https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-300x300.jpg\" class=\"attachment-medium size-medium wp-image-1133\" alt=\"\" srcset=\"https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-300x300.jpg 300w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-1024x1024.jpg 1024w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-150x150.jpg 150w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-768x768.jpg 768w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-1536x1536.jpg 1536w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-12x12.jpg 12w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-830x830.jpg 830w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-230x230.jpg 230w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-350x350.jpg 350w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478-480x480.jpg 480w, https:\/\/conexoesamazonicas.org\/wp-content\/uploads\/2021\/02\/IMG_20191005_134845290-scaled-1-e1621010646478.jpg 1920w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-4ae53bd4 elementor-widget elementor-widget-text-editor\" data-id=\"4ae53bd4\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p style=\"text-align: center;\">Adriana Moreira is an Environmental Engineer (FACET-MG), Master in Remote Sensing and PhD student in Water Resources and Environmental Sanitation (IPH\/UFRGS). More information on\u00a0<a href=\"http:\/\/lattes.cnpq.br\/2821011048854639\" target=\"_blank\" rel=\"noopener\">Lattes<\/a>\u00a0and\u00a0<a href=\"https:\/\/www.researchgate.net\/profile\/Adriana_Moreira6\" target=\"_blank\" rel=\"noopener\">ResearchGate<\/a>.\u00a0<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-8a18f15 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"8a18f15\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-66fc31a\" data-id=\"66fc31a\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-6b43c70 elementor-widget-divider--view-line elementor-widget elementor-widget-divider\" data-id=\"6b43c70\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\">\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-b9d5a76 elementor-widget elementor-widget-heading\" data-id=\"b9d5a76\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h4 class=\"elementor-heading-title elementor-size-default\">Leia tamb\u00e9m<\/h4>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-d97342a elementor-align-right elementor-widget elementor-widget-button\" data-id=\"d97342a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"button.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div class=\"elementor-button-wrapper\">\n\t\t\t\t\t<a class=\"elementor-button elementor-button-link elementor-size-sm\" href=\"#\">\n\t\t\t\t\t\t<span class=\"elementor-button-content-wrapper\">\n\t\t\t\t\t\t<span class=\"elementor-button-icon\">\n\t\t\t\t<i aria-hidden=\"true\" class=\"icon icon-left-arrows\"><\/i>\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t<span class=\"elementor-button-text\"> Voltar<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-151079f elementor-widget elementor-widget-html\" data-id=\"151079f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"html.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<script type=\"text\/javascript\">\r\n\r\njQuery(document).ready(function() {\r\n    jQuery('#wph-back-button').on('click', function() {\r\n      window.history.go(-1);\r\n      return false;\r\n    });\r\n});\r\n\r\n<\/script>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Vamos quantificar o ciclo da \u00e1gua? 04 de fevereiro de 2021 | Tempo de leitura: 8 minutos Por Adriana Moreira Temos ouvido falar que a floresta amaz\u00f4nica \u00e9 de extrema import\u00e2ncia para o clima regional e global. Mas como isso [&hellip;]<\/p>\n","protected":false},"author":8,"featured_media":1127,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"elementor_header_footer","format":"standard","meta":{"footnotes":""},"categories":[71],"tags":[78,45],"class_list":["post-14488","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-blog-conexoes-amazonicas","tag-78","tag-blog"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/posts\/14488","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/users\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/comments?post=14488"}],"version-history":[{"count":2,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/posts\/14488\/revisions"}],"predecessor-version":[{"id":14571,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/posts\/14488\/revisions\/14571"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/media\/1127"}],"wp:attachment":[{"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/media?parent=14488"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/categories?post=14488"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/conexoesamazonicas.org\/en\/wp-json\/wp\/v2\/tags?post=14488"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}