{"id":367,"date":"2023-06-15T14:39:37","date_gmt":"2023-06-15T14:39:37","guid":{"rendered":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/"},"modified":"2023-06-15T14:40:28","modified_gmt":"2023-06-15T14:40:28","slug":"roberta-dagostino","status":"publish","type":"page","link":"https:\/\/www.paleoclima.cnr.it\/en\/roberta-dagostino\/","title":{"rendered":"Roberta D\u2019Agostino"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"367\" class=\"elementor elementor-367 elementor-362\" data-elementor-post-type=\"page\">\n\t\t\t\t<div class=\"elementor-element elementor-element-bc7080d e-flex e-con-boxed e-con e-parent\" data-id=\"bc7080d\" 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-890ad65 elementor-widget elementor-widget-template\" data-id=\"890ad65\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"template.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-template\">\n\t\t\t\t\t<div data-elementor-type=\"page\" data-elementor-id=\"248\" class=\"elementor elementor-248\" data-elementor-post-type=\"elementor_library\">\n\t\t\t\t<div class=\"elementor-element elementor-element-97fc6aa e-flex e-con-boxed e-con e-parent\" data-id=\"97fc6aa\" 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-edf17d1 elementor-widget elementor-widget-image\" data-id=\"edf17d1\" 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=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg\" class=\"attachment-large size-large wp-image-169\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/>\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-a394913 elementor-widget elementor-widget-text-editor\" data-id=\"a394913\" 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<b>Roberta D\u2019Agostino<\/b> is a research scientist in Climate Dynamics at CNR-ISAC, Lecce since 2022.\r\n<br><br>She hs completed the PhD in Ecology and Climate Change at University of Salento in 2016. There, she investigated the response of tropical atmospheric circulation to a wide range external forcing in climate model simulations, spanning from the Last Glacial Maximum to Mid-Holocene conditions and future global warming scenarios. Afterwards, she moved as research fellow at ETH Z\u00fcrich continuing her work on large scale atmospheric dynamics. Roberta&#8217;s main postdoctoral activities has been carried out at Max-Planck-Institute f\u00fcr Meteorologie in Hamburg (2016 \u2013 2022). She has spent 6 years working in both Land and Ocean Departments, focusing on Holocene monsoon variability, seeking for emergent constraints linking past and future precipitation response. Before moving permanently to Lecce, she has been hired at University of Trento (2022) as RTD-a in Environmental, Mechanics and Civil Engineering Department, where she explored tropical Atlantic precipitation and global monsoons in the newest developed Storm Resolving Earth System Models.   \r\n<br><br>Since 2019 she is convener at European Geoscience Union General Assembly (Global monsoons and Energy and Dynamics in the Earth System sessions). She has been selected as Expert Reviewer for IPCC 6th Assessment Report, she is editor for \u201cFrontiers in Climate\u201d and she is serving as reviewer for major scientific journals (Science, Nature Communication, Nature Climate Change, Nature Geoscience, Scientific Report, Journal of Climate, Geophysical Research Letters, Environmental Research Letters, Climate Dynamics&#8230;). Furthermore, Roberta is qualified as Associate Professor in A4\/04 &#8211; GEO12 since 2022. She has taught Climate Modelling and Monitoring at University of Venice Ca&#8217; Foscari, and Introduction to Climate Change at University of Trento, with experience in supervising Master and PhD students. She has been invited for visiting periods at various international institutions (California Institute of Technology, United States, University of Reading, United Kingdom, Japan Meteorological Agency, Bureau of Meteorology, Australia).\r\n<br><br>Her main research activity is devoted to understand mechanisms for large-scale atmospheric circulation and hydrological budget response to different external forcing in past, present and future climate model simulations, with a particular emphasis on Hadley Circulation, monsoons and Mediterranean climate.\r\nShe is currently investigating the impact of internal variability and external forcing (e.g. GHG, aerosols, volcanic eruptions, dust, land-use change) on monsoon dynamics and megadroughts in regions with Mediterranean-like climates.\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-245c08a elementor-widget elementor-widget-template\" data-id=\"245c08a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"template.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-template\">\n\t\t\t\t\t<div data-elementor-type=\"page\" data-elementor-id=\"126\" class=\"elementor elementor-126\" data-elementor-post-type=\"elementor_library\">\n\t\t\t\t<div class=\"elementor-element elementor-element-ac2b398 e-flex e-con-boxed e-con e-parent\" data-id=\"ac2b398\" 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-4e40e91 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"4e40e91\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/eleonora-regattieri\/\" tabindex=\"-1\"><img decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo12.jpg\" class=\"attachment-full size-full wp-image-113\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo12.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo12-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo12-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/eleonora-regattieri\/\">Eleonora Regattieri<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IGG\n<br>(Coordinatrice)\n<br>(Geochimica, paleoclimatologia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-3001a37 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"3001a37\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/biagio-giaccio\/\" tabindex=\"-1\"><img decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo5.jpg\" class=\"attachment-full size-full wp-image-106\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo5.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo5-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo5-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/biagio-giaccio\/\">Biagio Giaccio<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IGAG\n<br>(Vide-Coordinatore)\n<br>(Tefrocronologia, stratigrafia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-57c8ce1 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"57c8ce1\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo4.jpg\" class=\"attachment-full size-full wp-image-105\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo4.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo4-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo4-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\">Roberto Bellucci<\/h3><p class=\"elementor-image-box-description\">CNR-DSSTTA\n<br>(Segreteria tecnico-scientifica)<\/p><\/div><\/div>\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<div class=\"elementor-element elementor-element-fb6e5ba e-grid e-con-boxed e-con e-parent\" data-id=\"fb6e5ba\" 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-d451712 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"d451712\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/alessandra-asioli\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo3.jpg\" class=\"attachment-full size-full wp-image-104\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo3.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo3-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo3-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/alessandra-asioli\/\">Alessandra Asioli<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISMAR\n<br>(Micropaleontologia, \npaleoceanografia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-917e365 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"917e365\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/carlo-baroni\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo7.jpg\" class=\"attachment-full size-full wp-image-108\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo7.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo7-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo7-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/carlo-baroni\/\">Carlo Baroni<\/a><\/h3><p class=\"elementor-image-box-description\">Universit\u00e0 di Pisa\n<br>(Geomorfologo, geologo glaciale)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f1cd2d6 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"f1cd2d6\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/michele-brunetti\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo14.jpg\" class=\"attachment-full size-full wp-image-115\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo14.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo14-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo14-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/michele-brunetti\/\">Michele Brunetti<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISAC\n<br>(Fisica, climatologia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-65937a0 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"65937a0\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/lucilla-capotondi\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo17.jpg\" class=\"attachment-full size-full wp-image-118\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo17.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo17-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo17-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/lucilla-capotondi\/\">Lucilla Capotondi<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISMAR\n<br>(Biostratigrafia, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-ec6788a elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"ec6788a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/francesco-cavalcante\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo8.jpg\" class=\"attachment-full size-full wp-image-109\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo8.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo8-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo8-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/francesco-cavalcante\/\">Francesco Cavalcante<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IMAA\n<br>(Mineralogia delle argille)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-312f140 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"312f140\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/irene-cornacchia\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo10.jpg\" class=\"attachment-full size-full wp-image-111\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo10.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo10-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo10-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/irene-cornacchia\/\">Irene Cornacchia<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IGAG\n<br>(Stratigrafia, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-ce797a2 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"ce797a2\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg\" class=\"attachment-full size-full wp-image-112\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/\">Roberta D\u2019agostino<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISAC\n<br>(Modellistica paleoclimatica)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-048fe3f elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"048fe3f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/donatella-domenica-insinga\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo16.jpg\" class=\"attachment-full size-full wp-image-117\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo16.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo16-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo16-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/donatella-domenica-insinga\/\">Donatella Domenica Insinga<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISMAR\n<br>(Tefrocronologia, geologia marina)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e239505 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"e239505\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/andrea-lami\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo2.jpg\" class=\"attachment-full size-full wp-image-103\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo2.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo2-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo2-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/andrea-lami\/\">Andrea Lami<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IRSA\n<br>(Paleolimnologia, biomarker)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f235d8e elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"f235d8e\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/fabrizio-lirer\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo13.jpg\" class=\"attachment-full size-full wp-image-114\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo13.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo13-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo13-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/fabrizio-lirer\/\">Fabrizio Lirer<\/a><\/h3><p class=\"elementor-image-box-description\">Universit\u00e0 Sapienza\n<br>(Biostratigrafia, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1b88df1 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"1b88df1\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/giovanni-monegato\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo19.jpg\" class=\"attachment-full size-full wp-image-120\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo19.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo19-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo19-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/giovanni-monegato\/\">Giovanni Monegato<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IGG\n<br>(Geologia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5e4ca56 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"5e4ca56\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/paolo-montagna\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo20.jpg\" class=\"attachment-full size-full wp-image-121\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo20.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo20-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo20-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/paolo-montagna\/\">Paolo Montagna<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISP\n<br>(Geochimica, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-83ff94c elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"83ff94c\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/cesare-ravazzi\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo9.jpg\" class=\"attachment-full size-full wp-image-110\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo9.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo9-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo9-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/cesare-ravazzi\/\">Cesare Ravazzi<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-IGAG\n<br>(Ecologia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e22d0b9 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"e22d0b9\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/prof-dr-barbara-stenni\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo21.jpg\" class=\"attachment-full size-full wp-image-122\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo21.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo21-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo21-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/prof-dr-barbara-stenni\/\">Barbara Stenni<\/a><\/h3><p class=\"elementor-image-box-description\">Universit\u00e0 C\u00e0 Foscari Venezia\n<br>(Geochimica, paleoclimatologa)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-bef1325 elementor-position-top elementor-widget elementor-widget-image-box\" data-id=\"bef1325\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.paleoclima.cnr.it\/chunxue-yang\/\" tabindex=\"-1\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo15.jpg\" class=\"attachment-full size-full wp-image-116\" alt=\"\" srcset=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo15.jpg 500w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo15-300x300.jpg 300w, https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo15-150x150.jpg 150w\" sizes=\"(max-width: 500px) 100vw, 500px\" \/><\/a><\/figure><div class=\"elementor-image-box-content\"><h3 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.paleoclima.cnr.it\/chunxue-yang\/\">Chunxue  Yang<\/a><\/h3><p class=\"elementor-image-box-description\">CNR-ISMAR\n<br>(Dinamica climatica, Modelli climatici)<\/p><\/div><\/div>\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>\n\t\t\t\t<\/div>\n\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>\n\t\t\t\t<\/div>\n\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>\n\t\t","protected":false},"excerpt":{"rendered":"<p><b>Roberta D\u2019Agostino<\/b> is a research scientist in Climate Dynamics at CNR-ISAC, Lecce since 2022.<\/p>\n<p>She hs completed the PhD in Ecology and Climate Change at University of Salento in 2016. There, she investigated the response of tropical atmospheric circulation to a wide range external forcing in climate model simulations, spanning from the Last Glacial Maximum to Mid-Holocene conditions and future global warming scenarios. Afterwards, she moved as research fellow at ETH Z\u00fcrich continuing her work on large scale atmospheric dynamics. Roberta&#8217;s main postdoctoral activities has been carried out at Max-Planck-Institute f\u00fcr Meteorologie in Hamburg (2016 \u2013 2022). She has spent 6 years working in both Land and Ocean Departments, focusing on Holocene monsoon variability, seeking for emergent constraints linking past and future precipitation response. Before moving permanently to Lecce, she has been hired at University of Trento (2022) as RTD-a in Environmental, Mechanics and Civil Engineering Department, where she explored tropical Atlantic precipitation and global monsoons in the newest developed Storm Resolving Earth System Models.   <\/p>\n<p>Since 2019 she is convener at European Geoscience Union General Assembly (Global monsoons and Energy and Dynamics in the Earth System sessions). She has been selected as Expert Reviewer for IPCC 6th Assessment Report, she is editor for \u201cFrontiers in Climate\u201d and she is serving as reviewer for major scientific journals (Science, Nature Communication, Nature Climate Change, Nature Geoscience, Scientific Report, Journal of Climate, Geophysical Research Letters, Environmental Research Letters, Climate Dynamics&#8230;). Furthermore, Roberta is qualified as Associate Professor in A4\/04 &#8211; GEO12 since 2022. She has taught Climate Modelling and Monitoring at University of Venice Ca&#8217; Foscari, and Introduction to Climate Change at University of Trento, with experience in supervising Master and PhD students. She has been invited for visiting periods at various international institutions (California Institute of Technology, United States, University of Reading, United Kingdom, Japan Meteorological Agency, Bureau of Meteorology, Australia).<\/p>\n<p>Her main research activity is devoted to understand mechanisms for large-scale atmospheric circulation and hydrological budget response to different external forcing in past, present and future climate model simulations, with a particular emphasis on Hadley Circulation, monsoons and Mediterranean climate.<br \/>\nShe is currently investigating the impact of internal variability and external forcing (e.g. GHG, aerosols, volcanic eruptions, dust, land-use change) on monsoon dynamics and megadroughts in regions with Mediterranean-like climates.<\/p>\n","protected":false},"author":1,"featured_media":169,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"elementor_header_footer","meta":{"footnotes":""},"class_list":["post-367","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Roberta D\u2019Agostino - CNR Paleoclima<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Roberta D\u2019Agostino - CNR Paleoclima\" \/>\n<meta property=\"og:description\" content=\"Roberta D\u2019Agostino is a research scientist in Climate Dynamics at CNR-ISAC, Lecce since 2022. She hs completed the PhD in Ecology and Climate Change at University of Salento in 2016. There, she investigated the response of tropical atmospheric circulation to a wide range external forcing in climate model simulations, spanning from the Last Glacial Maximum to Mid-Holocene conditions and future global warming scenarios. Afterwards, she moved as research fellow at ETH Z\u00fcrich continuing her work on large scale atmospheric dynamics. Roberta&#039;s main postdoctoral activities has been carried out at Max-Planck-Institute f\u00fcr Meteorologie in Hamburg (2016 \u2013 2022). She has spent 6 years working in both Land and Ocean Departments, focusing on Holocene monsoon variability, seeking for emergent constraints linking past and future precipitation response. Before moving permanently to Lecce, she has been hired at University of Trento (2022) as RTD-a in Environmental, Mechanics and Civil Engineering Department, where she explored tropical Atlantic precipitation and global monsoons in the newest developed Storm Resolving Earth System Models.   Since 2019 she is convener at European Geoscience Union General Assembly (Global monsoons and Energy and Dynamics in the Earth System sessions). She has been selected as Expert Reviewer for IPCC 6th Assessment Report, she is editor for \u201cFrontiers in Climate\u201d and she is serving as reviewer for major scientific journals (Science, Nature Communication, Nature Climate Change, Nature Geoscience, Scientific Report, Journal of Climate, Geophysical Research Letters, Environmental Research Letters, Climate Dynamics...). Furthermore, Roberta is qualified as Associate Professor in A4\/04 - GEO12 since 2022. She has taught Climate Modelling and Monitoring at University of Venice Ca&#039; Foscari, and Introduction to Climate Change at University of Trento, with experience in supervising Master and PhD students. She has been invited for visiting periods at various international institutions (California Institute of Technology, United States, University of Reading, United Kingdom, Japan Meteorological Agency, Bureau of Meteorology, Australia). Her main research activity is devoted to understand mechanisms for large-scale atmospheric circulation and hydrological budget response to different external forcing in past, present and future climate model simulations, with a particular emphasis on Hadley Circulation, monsoons and Mediterranean climate. She is currently investigating the impact of internal variability and external forcing (e.g. GHG, aerosols, volcanic eruptions, dust, land-use change) on monsoon dynamics and megadroughts in regions with Mediterranean-like climates.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/\" \/>\n<meta property=\"og:site_name\" content=\"CNR Paleoclima\" \/>\n<meta property=\"article:modified_time\" content=\"2023-06-15T14:40:28+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"500\" \/>\n\t<meta property=\"og:image:height\" content=\"500\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/\",\"name\":\"Roberta D\u2019Agostino - CNR Paleoclima\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/#primaryimage\"},\"image\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/chi-siamo11.jpg\",\"datePublished\":\"2023-06-15T14:39:37+00:00\",\"dateModified\":\"2023-06-15T14:40:28+00:00\",\"breadcrumb\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/#primaryimage\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/chi-siamo11.jpg\",\"contentUrl\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/chi-siamo11.jpg\",\"width\":500,\"height\":500},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/roberta-dagostino\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Roberta D\u2019Agostino\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#website\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/\",\"name\":\"CNR Paleoclima\",\"description\":\"\",\"publisher\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#organization\"},\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"},{\"@type\":\"Organization\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#organization\",\"name\":\"CNR Paleoclima\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/\",\"logo\":{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#\\\/schema\\\/logo\\\/image\\\/\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/cropped-logo2.png\",\"contentUrl\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/cropped-logo2.png\",\"width\":2479,\"height\":674,\"caption\":\"CNR Paleoclima\"},\"image\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#\\\/schema\\\/logo\\\/image\\\/\"}}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Roberta D\u2019Agostino - CNR Paleoclima","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/","og_locale":"en_US","og_type":"article","og_title":"Roberta D\u2019Agostino - CNR Paleoclima","og_description":"Roberta D\u2019Agostino is a research scientist in Climate Dynamics at CNR-ISAC, Lecce since 2022. She hs completed the PhD in Ecology and Climate Change at University of Salento in 2016. There, she investigated the response of tropical atmospheric circulation to a wide range external forcing in climate model simulations, spanning from the Last Glacial Maximum to Mid-Holocene conditions and future global warming scenarios. Afterwards, she moved as research fellow at ETH Z\u00fcrich continuing her work on large scale atmospheric dynamics. Roberta's main postdoctoral activities has been carried out at Max-Planck-Institute f\u00fcr Meteorologie in Hamburg (2016 \u2013 2022). She has spent 6 years working in both Land and Ocean Departments, focusing on Holocene monsoon variability, seeking for emergent constraints linking past and future precipitation response. Before moving permanently to Lecce, she has been hired at University of Trento (2022) as RTD-a in Environmental, Mechanics and Civil Engineering Department, where she explored tropical Atlantic precipitation and global monsoons in the newest developed Storm Resolving Earth System Models.   Since 2019 she is convener at European Geoscience Union General Assembly (Global monsoons and Energy and Dynamics in the Earth System sessions). She has been selected as Expert Reviewer for IPCC 6th Assessment Report, she is editor for \u201cFrontiers in Climate\u201d and she is serving as reviewer for major scientific journals (Science, Nature Communication, Nature Climate Change, Nature Geoscience, Scientific Report, Journal of Climate, Geophysical Research Letters, Environmental Research Letters, Climate Dynamics...). Furthermore, Roberta is qualified as Associate Professor in A4\/04 - GEO12 since 2022. She has taught Climate Modelling and Monitoring at University of Venice Ca' Foscari, and Introduction to Climate Change at University of Trento, with experience in supervising Master and PhD students. She has been invited for visiting periods at various international institutions (California Institute of Technology, United States, University of Reading, United Kingdom, Japan Meteorological Agency, Bureau of Meteorology, Australia). Her main research activity is devoted to understand mechanisms for large-scale atmospheric circulation and hydrological budget response to different external forcing in past, present and future climate model simulations, with a particular emphasis on Hadley Circulation, monsoons and Mediterranean climate. She is currently investigating the impact of internal variability and external forcing (e.g. GHG, aerosols, volcanic eruptions, dust, land-use change) on monsoon dynamics and megadroughts in regions with Mediterranean-like climates.","og_url":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/","og_site_name":"CNR Paleoclima","article_modified_time":"2023-06-15T14:40:28+00:00","og_image":[{"width":500,"height":500,"url":"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg","type":"image\/jpeg"}],"twitter_card":"summary_large_image","schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/","url":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/","name":"Roberta D\u2019Agostino - CNR Paleoclima","isPartOf":{"@id":"https:\/\/www.paleoclima.cnr.it\/#website"},"primaryImageOfPage":{"@id":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/#primaryimage"},"image":{"@id":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/#primaryimage"},"thumbnailUrl":"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg","datePublished":"2023-06-15T14:39:37+00:00","dateModified":"2023-06-15T14:40:28+00:00","breadcrumb":{"@id":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/"]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/#primaryimage","url":"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg","contentUrl":"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo11.jpg","width":500,"height":500},{"@type":"BreadcrumbList","@id":"https:\/\/www.paleoclima.cnr.it\/roberta-dagostino\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/www.paleoclima.cnr.it\/"},{"@type":"ListItem","position":2,"name":"Roberta D\u2019Agostino"}]},{"@type":"WebSite","@id":"https:\/\/www.paleoclima.cnr.it\/#website","url":"https:\/\/www.paleoclima.cnr.it\/","name":"CNR Paleoclima","description":"","publisher":{"@id":"https:\/\/www.paleoclima.cnr.it\/#organization"},"potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/www.paleoclima.cnr.it\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"},{"@type":"Organization","@id":"https:\/\/www.paleoclima.cnr.it\/#organization","name":"CNR Paleoclima","url":"https:\/\/www.paleoclima.cnr.it\/","logo":{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.paleoclima.cnr.it\/#\/schema\/logo\/image\/","url":"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/cropped-logo2.png","contentUrl":"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/cropped-logo2.png","width":2479,"height":674,"caption":"CNR Paleoclima"},"image":{"@id":"https:\/\/www.paleoclima.cnr.it\/#\/schema\/logo\/image\/"}}]}},"_links":{"self":[{"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/pages\/367","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/comments?post=367"}],"version-history":[{"count":1,"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/pages\/367\/revisions"}],"predecessor-version":[{"id":368,"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/pages\/367\/revisions\/368"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/media\/169"}],"wp:attachment":[{"href":"https:\/\/www.paleoclima.cnr.it\/en\/wp-json\/wp\/v2\/media?parent=367"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}