{"id":19867,"date":"2022-03-03T13:39:52","date_gmt":"2022-03-03T16:39:52","guid":{"rendered":"http:\/\/www.cr2.cl\/eng\/?p=19867"},"modified":"2022-03-11T13:42:29","modified_gmt":"2022-03-11T16:42:29","slug":"a-salt-bath-in-bolivia-nasa-earth-observatory","status":"publish","type":"post","link":"https:\/\/www.cr2.cl\/eng\/a-salt-bath-in-bolivia-nasa-earth-observatory\/","title":{"rendered":"A Salt Bath in Bolivia (Nasa Earth Observatory)"},"content":{"rendered":"<p>Bolivia\u2019s Salar de Uyuni is the largest salt flat (or playa) in the world. For much of the year, it stretches out in a seemingly endless <a href=\"https:\/\/earthobservatory.nasa.gov\/images\/144826\/salt-flats-mountains-and-moisture\">expanse of white<\/a>, with a salt crust covering 10,000 square kilometers (4,000 square miles). During the rainy season, water can fill part of the salt flat and give it a stunning, mirror-like appearance. In early 2022, that watery mirror grew larger and lingered longer than it has in several years.<\/p>\n<p>Abundant rainfall around the <a href=\"https:\/\/www.earthmagazine.org\/article\/travels-geology-sky-high-adventure-bolivias-altiplano\/\">Altiplano<\/a> in <a href=\"https:\/\/senamhi.gob.bo\/climatologia\/11_RESUMEN_CLIMATICO_NOVIEMBRE.pdf\">November<\/a>, <a href=\"http:\/\/senamhi.gob.bo\/climatologia\/12_RESUMEN_CLIMATICO_DICIEMBRE.pdf\">December<\/a>, and early <a href=\"http:\/\/senamhi.gob.bo\/climatologia\/01_RESUMEN_CLIMATICO_ENERO_2022.pdf\">January<\/a> had the Salar de Uyuni brimming with water nearly to its edges. In fact, <a href=\"https:\/\/correodelsur.com\/sociedad\/20220105_limitan-acceso-al-salar-de-uyuni-por-las-inundaciones.html\">local newspapers reported<\/a> flooding in some areas and temporary prohibitions on travel across the salar during the busy tourist season.<\/p>\n<p>\u201cThe extent of the filling of Salar de Uyuni this year is above normal. The rainy season started earlier than previous years, and rainfall was well above average over the southern Altiplano,\u201d said hydrologist Jorge Molina Carpio of the Universidad Mayor de San Andr\u00e9s. \u201cThis was probably related to the onset of a significant <a href=\"https:\/\/earthobservatory.nasa.gov\/images\/149201\/la-nina-returns-for-a-second-winter\">La Ni\u00f1a event<\/a>. Strong La Ni\u00f1as during the rainy season are related to positive rainfall anomalies in the southern Altiplano.\u201d<\/p>\n<p>The false-color images above were acquired by NASA\u2019s <a href=\"https:\/\/aqua.nasa.gov\/\">Aqua<\/a> satellite on August 22, 2021, and NASA\u2019s <a href=\"https:\/\/terra.nasa.gov\/\">Terra<\/a> satellite on February 19, 2022. Each satellite used its <a href=\"https:\/\/modis.gsfc.nasa.gov\/about\/\">Moderate Resolution Imaging Spectroradiometer<\/a> (MODIS). The images were composed from a combination of visible light, near-infrared, and shortwave infrared (MODIS bands 7-2-1) to better distinguish standing water (blue and dark blue) from clouds (white) and the salt flats (shades of teal).<\/p>\n<div class=\"panel image-viewer-panel\">\n<div class=\"panel-image\"><a href=\"https:\/\/eoimages.gsfc.nasa.gov\/images\/imagerecords\/149000\/149502\/salardeuyuni_oli_202231_lrg.jpg\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class=\"td-animation-stack-type0-2\" src=\"https:\/\/eoimages.gsfc.nasa.gov\/images\/imagerecords\/149000\/149502\/salardeuyuni_oli_202231.jpg\" alt=\"\" \/><\/a><\/div>\n<div class=\"panel-footer\">\n<p class=\"first\">January 31, 2022<a class=\"download-btn download-btn-first no-underline pull-right hvr-rectangle-out\" href=\"https:\/\/eoimages.gsfc.nasa.gov\/images\/imagerecords\/149000\/149502\/salardeuyuni_oli_202231_lrg.jpg\" target=\"_blank\" rel=\"noopener noreferrer\">JPEG<\/a><\/p>\n<div class=\"clearfix\"><\/div>\n<\/div>\n<\/div>\n<div class=\"panel image-viewer-panel\">\n<div class=\"panel-image\"><img decoding=\"async\" class=\"td-animation-stack-type0-2\" src=\"https:\/\/eoimages.gsfc.nasa.gov\/images\/imagerecords\/149000\/149502\/salardeuyunizm_oli_202231.jpg\" alt=\"\" \/><\/div>\n<div class=\"panel-footer\">\n<p class=\"first\">January 31, 2022<\/p>\n<div class=\"clearfix\"><\/div>\n<\/div>\n<\/div>\n<p>The natural-color images above were acquired on January 31, 2022, by the <a href=\"https:\/\/landsat.gsfc.nasa.gov\/satellites\/landsat-8\/spacecraft-instruments\/operational-land-imager\/\">Operational Land Imager<\/a> (OLI) on <a href=\"https:\/\/landsat.gsfc.nasa.gov\/satellites\/landsat-8\/\">Landsat 8<\/a>. Note the discoloration of the water and the salt flat, which could be due to a combination of runoff, volcanic sediments, and microbes or algae thriving in the water.<\/p>\n<p>\u201cAlong the Altiplano, but especially in its southwestern edge, precipitation is largely concentrated in austral summer, when transient periods of intense convection are fueled by moisture from the Bolivian lowlands and Amazon basin. The rest of the year is bone dry,\u201d said Ren\u00e9 Garreaud, a climate scientist at the University of Chile. High-level winds, which vary from season to season and with La Ni\u00f1a and El Ni\u00f1o events, control when and how much moist air rides up onto the plateau. \u201cThe stronger and more persistent the easterly wind, the more precipitation you get over the Altiplano.\u201d<\/p>\n<p>Garreaud noted that there was a strong easterly flow over the central Andes in December 2021 and early January 2022, leading to abundant rain in the Uyuni-Potosi region. \u201cThis area is a closed basin, so all of the precipitation\u2014as rain at the valley floor and snow over the surrounding peaks\u2014contributes to the filling of the Uyuni and <a href=\"https:\/\/earthobservatory.nasa.gov\/images\/79347\/salar-de-coipasa-bolivia\">Coipasa<\/a> dry lakes,\u201d he added.<\/p>\n<p>Salar de Uyuni is rich in minerals\u2014especially lithium (used in batteries), halite (common table salt), and ulexite and gypsum (for fertilizer and plaster)\u2014some of which have been harvested here since at least the 1600s. The stunningly flat landscape draws many tourists who come to see the salty crust in the dry season and the mirror lakes in the wet season. The salt flat is also popular with remote sensing scientists, who use the landscape to calibrate satellite imagers and altimeters.<\/p>\n<p><i>NASA Earth Observatory images by Lauren Dauphin, using Landsat data from the <a href=\"http:\/\/earthexplorer.usgs.gov\">U.S. Geological Survey<\/a> and NASA Earth Observatory image by NAME, using MODIS data from NASA EOSDIS <a href=\"https:\/\/earthdata.nasa.gov\/lance\">LANCE<\/a> and <a href=\"https:\/\/worldview.earthdata.nasa.gov\/\">GIBS\/Worldview<\/a>. Story by <a href=\"https:\/\/earthobservatory.nasa.gov\/about\/michael-carlowicz\">Michael Carlowicz<\/a>.<\/i><\/p>\n<p>Read at <a href=\"https:\/\/earthobservatory.nasa.gov\/images\/149502\/a-salt-bath-in-bolivia\">Nasa Earth Observatory<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Bolivia\u2019s Salar de Uyuni is the largest salt flat (or playa) in the world. For much of the year, it stretches out in a seemingly endless expanse of white, with a salt crust covering 10,000 square kilometers (4,000 square miles). During the rainy season, water can fill part of the salt flat and give it [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":19869,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[25],"tags":[],"_links":{"self":[{"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/posts\/19867"}],"collection":[{"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/comments?post=19867"}],"version-history":[{"count":1,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/posts\/19867\/revisions"}],"predecessor-version":[{"id":19868,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/posts\/19867\/revisions\/19868"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/media\/19869"}],"wp:attachment":[{"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/media?parent=19867"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/categories?post=19867"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.cr2.cl\/eng\/wp-json\/wp\/v2\/tags?post=19867"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}