{"id":1012016,"date":"2026-02-26T13:07:44","date_gmt":"2026-02-26T12:07:44","guid":{"rendered":"https:\/\/new.obsnev.es\/?post_type=protocolos&#038;p=1012016"},"modified":"2026-02-27T09:36:54","modified_gmt":"2026-02-27T08:36:54","slug":"caracterizacion-detallada-de-formaciones-vegetales-mediante-ortofotografia","status":"publish","type":"protocolos","link":"https:\/\/obsnev.es\/en\/protocolos\/caracterizacion-detallada-de-formaciones-vegetales-mediante-ortofotografia\/","title":{"rendered":"Detailed characterization of plant formations using orthophotography"},"content":{"rendered":"<div data-elementor-type=\"wp-post\" data-elementor-id=\"1012016\" class=\"elementor elementor-1012016\" data-elementor-post-type=\"protocolos\">\n\t\t\t\t<div class=\"elementor-element elementor-element-63787e3 e-flex e-con-boxed e-con e-parent\" data-id=\"63787e3\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-4db42ea elementor-widget elementor-widget-text-editor\" data-id=\"4db42ea\" 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<div id=\"panel-gb4326-69a033732152e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"0\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-0\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Aims<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><ul><li>To provide a detailed characterization of the changes in the main plant formations of Sierra Nevada.<\/li><li>To quantify the temporal variations in density and degree of coverage of the main species in relation to elevation.<\/li><\/ul><\/div><\/div><\/div><\/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-e2fa565 elementor-widget elementor-widget-image\" data-id=\"e2fa565\" 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 fetchpriority=\"high\" decoding=\"async\" width=\"992\" height=\"534\" src=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-1_ES.png\" class=\"attachment-2048x2048 size-2048x2048 wp-image-4338\" alt=\"\" srcset=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-1_ES.png 992w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-1_ES-300x161.png 300w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-1_ES-768x413.png 768w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-1_ES-18x10.png 18w\" sizes=\"(max-width: 992px) 100vw, 992px\" \/>\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-95f591f elementor-widget elementor-widget-text-editor\" data-id=\"95f591f\" 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<div id=\"panel-gb4326-69a033732152e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"0\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-0\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><div id=\"panel-gb4326-69a033732152e-0-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"2\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-2\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Method and effort<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>The detailed delineation of plant formations is superimposed over aerial orthorectified photographs of different dates (working scale 1:5,000-1:8,000). Certain zones within the distribution area of the formation are selected to make comparisons between dates, considering the availability of data as well as their quality. In these preselected areas, a series of 1-ha circular plots are randomly distributed. The individuals of the main species are counted and the coverage of this species estimated for the different dates.<\/p><p>In addition, a series of transects are laid out by photointerpretation according to an altitudinal gradient. Over each transect, tangential circles (the size is c. 30 m in radius) are drawn covering the distribution range of the oak forests and juniper thickets (1100 m to 2700 m). The working scale varies between 1:3,000 and 1:5,000. In these plots, the photointerpretation is made recording the variables of interest for each date.<\/p><\/div><\/div><\/div><\/div><\/div><\/div><\/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-cf1eb1c elementor-widget elementor-widget-image\" data-id=\"cf1eb1c\" 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=\"992\" height=\"755\" src=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-2_ES.png\" class=\"attachment-2048x2048 size-2048x2048 wp-image-4339\" alt=\"\" srcset=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-2_ES.png 992w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-2_ES-300x228.png 300w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-2_ES-768x585.png 768w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_1_2-2_ES-16x12.png 16w\" sizes=\"(max-width: 992px) 100vw, 992px\" \/>\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-6577262 elementor-widget elementor-widget-text-editor\" data-id=\"6577262\" 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<div id=\"panel-gb4326-69a033732152e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"0\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-0\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><div id=\"panel-gb4326-69a033732152e-0-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"2\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-2\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><div id=\"panel-gb4335-69a033861f4e4-0-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"2\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4335-69a033861f4e4-0-0-2\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Periodicity<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>At present, there are photos of Sierra Nevada of sufficient quality for the dates: 1956, 1977, 1984, 1998, 2001, 2004, 2007, and 2009.<\/p><\/div><\/div><\/div><\/div><div id=\"panel-gb4335-69a033861f4e4-0-0-3\" class=\"so-panel widget widget_sow-editor panel-last-child\" data-index=\"3\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4335-69a033861f4e4-0-0-3\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">References<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>Allen, C.D. y Breshears, D.D. 1998. Drought-induced shift of a forest-woodland ecotone: Rapid landscape response to climate variation. PNAS, 95 (25): 14839\u201314842<br \/>Navarro Gonz\u00e1lez, I. y Bonet Garc\u00eda, F.J. 2010. Vegetation cover changes in Sierra Nevada mountains (Spain) during the past 50 years and relation to land use and climate change. p. 53. En: 2\u00aa International GMBA-DIVERSITAS Conference \u201cFunctional significance of mountain biodiversity\u201d. Chandolin, Switzerland. 27 \u2013 30 Jul. Conference abstracts.<br \/>Sanz-Elorza, M., Dana, E., Gonz\u00e1lez, A. y Sobrino, E. 2003. Changes in the high-mountain vegetation of the central Iberian Peninsula as a probable sign of global warming. Ann. Bot., 92:273\u2013280.<\/p><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div>\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\t\t<\/div>\n\t\t\t\t<\/div>","protected":false},"featured_media":1012107,"template":"","meta":{"_acf_changed":false},"ambito-tematico":[345],"class_list":["post-1012016","protocolos","type-protocolos","status-publish","has-post-thumbnail","hentry","ambito-tematico-reconstruccion-del-pasado"],"acf":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos\/1012016","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos"}],"about":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/types\/protocolos"}],"version-history":[{"count":5,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos\/1012016\/revisions"}],"predecessor-version":[{"id":1012077,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos\/1012016\/revisions\/1012077"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/media\/1012107"}],"wp:attachment":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/media?parent=1012016"}],"wp:term":[{"taxonomy":"ambito-tematico","embeddable":true,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/ambito-tematico?post=1012016"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}