<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">R. Gentili</style></author><author><style face="normal" font="default" size="100%">C. Baroni</style></author><author><style face="normal" font="default" size="100%">C. Panigada</style></author><author><style face="normal" font="default" size="100%">M. Rossini</style></author><author><style face="normal" font="default" size="100%">G. Tagliabue</style></author><author><style face="normal" font="default" size="100%">S. Armiraglio</style></author><author><style face="normal" font="default" size="100%">S. Citterio</style></author><author><style face="normal" font="default" size="100%">A. Carton</style></author><author><style face="normal" font="default" size="100%">M.C. Salvatore</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacier shrinkage and slope processes create habitat at high elevation and microrefugia across treeline for alpine plants during warm stages</style></title><secondary-title><style face="normal" font="default" size="100%">Catena</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Evolutionary geomorphology</style></keyword><keyword><style  face="normal" font="default" size="100%">Glacier retreat</style></keyword><keyword><style  face="normal" font="default" size="100%">Microclimate</style></keyword><keyword><style  face="normal" font="default" size="100%">Periglacial refugia</style></keyword><keyword><style  face="normal" font="default" size="100%">Satellite remote sensing</style></keyword><keyword><style  face="normal" font="default" size="100%">Species’ resilienc</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">04/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.catena.2020.104626</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">193</style></volume><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">A. Cascella</style></author><author><style face="normal" font="default" size="100%">S. Bonomo</style></author><author><style face="normal" font="default" size="100%">B. Jalali</style></author><author><style face="normal" font="default" size="100%">M.A. Sicre</style></author><author><style face="normal" font="default" size="100%">N. Pelosi</style></author><author><style face="normal" font="default" size="100%">S. Schmidt</style></author><author><style face="normal" font="default" size="100%">F. Lirer</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences</style></title><secondary-title><style face="normal" font="default" size="100%">The Holocene</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Central Mediterranean</style></keyword><keyword><style  face="normal" font="default" size="100%">coccolithophores</style></keyword><keyword><style  face="normal" font="default" size="100%">coccolithophorid primary productivity</style></keyword><keyword><style  face="normal" font="default" size="100%">last millennia</style></keyword><keyword><style  face="normal" font="default" size="100%">reworked coccoliths</style></keyword><keyword><style  face="normal" font="default" size="100%">South Adriatic Sea</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">07/2019</style></date></pub-dates></dates><volume><style face="normal" font="default" size="100%">1-12</style></volume><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">M. Rinaldi</style></author><author><style face="normal" font="default" size="100%">A. Nicosia</style></author><author><style face="normal" font="default" size="100%">G. Santachiara</style></author><author><style face="normal" font="default" size="100%">M. Piazza</style></author><author><style face="normal" font="default" size="100%">M. Paglione</style></author><author><style face="normal" font="default" size="100%">S. Gilardoni</style></author><author><style face="normal" font="default" size="100%">S. Sandrini</style></author><author><style face="normal" font="default" size="100%">P. Cristofanelli</style></author><author><style face="normal" font="default" size="100%">A. Marinoni</style></author><author><style face="normal" font="default" size="100%">P. Bonasoni</style></author><author><style face="normal" font="default" size="100%">M.C. Facchini</style></author><author><style face="normal" font="default" size="100%">F. Belosi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Ground level ice nucleating particles measurements at Capo Granitola, a Mediterranean coastal site</style></title><secondary-title><style face="normal" font="default" size="100%">Atmospheric Research</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Heterogeneous freezing</style></keyword><keyword><style  face="normal" font="default" size="100%">Ice nucleating particles</style></keyword><keyword><style  face="normal" font="default" size="100%">Particle number concentration</style></keyword><keyword><style  face="normal" font="default" size="100%">Saharan dust transport</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">05/2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.atmosres.2018.12.022</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">219</style></volume><pages><style face="normal" font="default" size="100%">57-64</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">P. Cristofanelli</style></author><author><style face="normal" font="default" size="100%">P. Di Carlo</style></author><author><style face="normal" font="default" size="100%">E. Aruffo</style></author><author><style face="normal" font="default" size="100%">F. Apadula</style></author><author><style face="normal" font="default" size="100%">M. Bencardino</style></author><author><style face="normal" font="default" size="100%">F. D'Amore</style></author><author><style face="normal" font="default" size="100%">P. Bonasoni</style></author><author><style face="normal" font="default" size="100%">D. Putero</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">An Assessment of Stratospheric Intrusions in Italian Mountain Regions Using STEFLUX</style></title><secondary-title><style face="normal" font="default" size="100%">Atmosphere</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Mediterranean Basin</style></keyword><keyword><style  face="normal" font="default" size="100%">mountain regions</style></keyword><keyword><style  face="normal" font="default" size="100%">ozone</style></keyword><keyword><style  face="normal" font="default" size="100%">stratosphere-to-troposphere transport</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2018</style></year><pub-dates><date><style  face="normal" font="default" size="100%">10/2018</style></date></pub-dates></dates><volume><style face="normal" font="default" size="100%">9</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">10</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Leonelli, Giovanni</style></author><author><style face="normal" font="default" size="100%">Battipaglia, Giovanna</style></author><author><style face="normal" font="default" size="100%">Cherubini, Paolo</style></author><author><style face="normal" font="default" size="100%">Saurer, Matthias</style></author><author><style face="normal" font="default" size="100%">Siegwolf, Rolf T V</style></author><author><style face="normal" font="default" size="100%">Maugeri, Maurizio</style></author><author><style face="normal" font="default" size="100%">Stenni, Barbara</style></author><author><style face="normal" font="default" size="100%">Fusco, Stella</style></author><author><style face="normal" font="default" size="100%">Maggi, Valter</style></author><author><style face="normal" font="default" size="100%">Pelfini, Manuela</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Larix decidua δ18O tree-ring cellulose mainly reflects the isotopic signature of winter snow in a high-altitude glacial valley of the European Alps</style></title><secondary-title><style face="normal" font="default" size="100%">Science of the Total Environment</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Dendroclimatology</style></keyword><keyword><style  face="normal" font="default" size="100%">Dendroecology</style></keyword><keyword><style  face="normal" font="default" size="100%">European larch</style></keyword><keyword><style  face="normal" font="default" size="100%">Stable isotopes</style></keyword><keyword><style  face="normal" font="default" size="100%">Tree rings</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1016/j.scitotenv.2016.11.129</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">579</style></volume><pages><style face="normal" font="default" size="100%">230-237</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Alberico, I</style></author><author><style face="normal" font="default" size="100%">Giliberti, I</style></author><author><style face="normal" font="default" size="100%">Insinga, D D</style></author><author><style face="normal" font="default" size="100%">Petrosino, P</style></author><author><style face="normal" font="default" size="100%">Vallefuoco, M</style></author><author><style face="normal" font="default" size="100%">Lirer, F</style></author><author><style face="normal" font="default" size="100%">Bonomo, S</style></author><author><style face="normal" font="default" size="100%">Cascella, A</style></author><author><style face="normal" font="default" size="100%">Anzalone, E</style></author><author><style face="normal" font="default" size="100%">Barra, E</style></author><author><style face="normal" font="default" size="100%">Marsella, E</style></author><author><style face="normal" font="default" size="100%">Ferraro, L</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Marine sediment cores database for the Mediterranean Basin: a tool for past climatic and environmental studies</style></title><secondary-title><style face="normal" font="default" size="100%">Open Geosciences</style></secondary-title><short-title><style face="normal" font="default" size="100%">Open Geosci.</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">climatic paleoproxies</style></keyword><keyword><style  face="normal" font="default" size="100%">database</style></keyword><keyword><style  face="normal" font="default" size="100%">marine sediment cores</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean Sea</style></keyword><keyword><style  face="normal" font="default" size="100%">spatial analysis</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2017</style></year><pub-dates><date><style  face="normal" font="default" size="100%">03/2017</style></date></pub-dates></dates><volume><style face="normal" font="default" size="100%">9</style></volume><pages><style face="normal" font="default" size="100%">221 - 239</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">I. Alberico</style></author><author><style face="normal" font="default" size="100%">I. Giliberti</style></author><author><style face="normal" font="default" size="100%">D.D. Insinga</style></author><author><style face="normal" font="default" size="100%">P. Petrosino</style></author><author><style face="normal" font="default" size="100%">M. Vallefuoco</style></author><author><style face="normal" font="default" size="100%">F. Lirer</style></author><author><style face="normal" font="default" size="100%">S. Bonomo</style></author><author><style face="normal" font="default" size="100%">A. Cascella</style></author><author><style face="normal" font="default" size="100%">E. Anzalone</style></author><author><style face="normal" font="default" size="100%">R. Barra</style></author><author><style face="normal" font="default" size="100%">E. Marsella</style></author><author><style face="normal" font="default" size="100%">L. Ferraro</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Marine sediment cores database for the Mediterranean Basin: a tool for past climatic environmental studies</style></title><secondary-title><style face="normal" font="default" size="100%">Open Geosciences</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">climatic paleoproxies</style></keyword><keyword><style  face="normal" font="default" size="100%">database</style></keyword><keyword><style  face="normal" font="default" size="100%">marine sediment cores</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean Sea</style></keyword><keyword><style  face="normal" font="default" size="100%">spatial analysis</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><volume><style face="normal" font="default" size="100%">9</style></volume><pages><style face="normal" font="default" size="100%">221-239</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Peano, Daniele</style></author><author><style face="normal" font="default" size="100%">Chiarle, Marta</style></author><author><style face="normal" font="default" size="100%">von Hardenberg, Jost</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A minimal model approach for glacier length modeling in the western Italian Alps</style></title><secondary-title><style face="normal" font="default" size="100%">Geografia Fisica e Dinamica Quaternaria</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Glaciers length reconstruction</style></keyword><keyword><style  face="normal" font="default" size="100%">Minimal glacier model</style></keyword><keyword><style  face="normal" font="default" size="100%">Surface mass balance</style></keyword><keyword><style  face="normal" font="default" size="100%">Western Italian Alps</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><volume><style face="normal" font="default" size="100%">39</style></volume><pages><style face="normal" font="default" size="100%">69–82</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;We study the response of a set of glaciers in the Western Italian Alps to climate variations using a minimal glacier modeling approach, first introduced by Oerlemans. The mathematical models are forced over the period 1959-2009, using temperature and precipitation recorded by a dense network of meteorological stations, and we find a good match between the observed and modeled glacier length dynamics, especially for the two glaciers that have observed surface mass balance, i.e. Ciardoney and Grand Etret, and, in absence of observed surface mass balance, for small glaciers, such as Basei, Bessanese, and Capra. Forcing the model with future projections from a state-of-the-art global climate model in the RCP 4.5 and RCP 8.5 scenarios, we show how this approach can be used to obtain a first estimate for the future evolution of these glaciers length and we discuss the related uncertainties.&lt;/p&gt;</style></abstract><work-type><style face="normal" font="default" size="100%">Article</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">P. Cristofanelli</style></author><author><style face="normal" font="default" size="100%">T.C. Landi</style></author><author><style face="normal" font="default" size="100%">F. Calzolari</style></author><author><style face="normal" font="default" size="100%">R. Duchi</style></author><author><style face="normal" font="default" size="100%">A. Marinoni</style></author><author><style face="normal" font="default" size="100%">M. Rinaldi</style></author><author><style face="normal" font="default" size="100%">P. Bonasoni</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Summer atmospheric composition over the Mediterranean basin: Investigation on transport processes and pollutant export to the free troposphere by observations at the WMO/GAW Mt. Cimone global station (Italy, 2165 m a.s.l.)</style></title><secondary-title><style face="normal" font="default" size="100%">Atmospheric Environment</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Air-mass age</style></keyword><keyword><style  face="normal" font="default" size="100%">Air-mass transport</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean Basin</style></keyword><keyword><style  face="normal" font="default" size="100%">Po basin</style></keyword><keyword><style  face="normal" font="default" size="100%">Short-lived climate forcers/pollutants</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2016</style></year><pub-dates><date><style  face="normal" font="default" size="100%">06/2016</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1016/j.atmosenv.2016.06.048</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">141</style></volume><pages><style face="normal" font="default" size="100%">139-152</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Balestrini, Raffaella</style></author><author><style face="normal" font="default" size="100%">Delconte, Carlo A</style></author><author><style face="normal" font="default" size="100%">Sacchi, Elisa</style></author><author><style face="normal" font="default" size="100%">Wilson Alana M</style></author><author><style face="normal" font="default" size="100%">Williams, Mark W</style></author><author><style face="normal" font="default" size="100%">Cristofanelli, Paolo</style></author><author><style face="normal" font="default" size="100%">Putero, Davide</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Wet deposition at the base of Mt Everest: Seasonal evolution of the chemistry and isotopic composition</style></title><secondary-title><style face="normal" font="default" size="100%">Atmospheric Environment</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Back-trajectories d-excess</style></keyword><keyword><style  face="normal" font="default" size="100%">Monsoon</style></keyword><keyword><style  face="normal" font="default" size="100%">Nitrate</style></keyword><keyword><style  face="normal" font="default" size="100%">Snow</style></keyword><keyword><style  face="normal" font="default" size="100%">Sulfate</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2016</style></year><pub-dates><date><style  face="normal" font="default" size="100%">08/2016</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1016/j.atmosenv.2016.08.056</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">146</style></volume><pages><style face="normal" font="default" size="100%">100-112</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">F Lirer</style></author><author><style face="normal" font="default" size="100%">M Sprovieri</style></author><author><style face="normal" font="default" size="100%">M Vallefuoco</style></author><author><style face="normal" font="default" size="100%">L Ferraro</style></author><author><style face="normal" font="default" size="100%">N Pelosi</style></author><author><style face="normal" font="default" size="100%">L Giordano</style></author><author><style face="normal" font="default" size="100%">L Capotondi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Planktonic foraminifera as bio-indicators for monitoring the climatic changes occurred during the last 2000 years in the SE Tyrrhenian Sea</style></title><secondary-title><style face="normal" font="default" size="100%">Integrative Zoology Journal</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Mediterranean Basin</style></keyword><keyword><style  face="normal" font="default" size="100%">oxygen stable isotopes</style></keyword><keyword><style  face="normal" font="default" size="100%">planktonic foraminifera</style></keyword><keyword><style  face="normal" font="default" size="100%">southeastern Tyrrhenian Sea</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><volume><style face="normal" font="default" size="100%">9</style></volume><pages><style face="normal" font="default" size="100%">542-554</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zampieri,M.</style></author><author><style face="normal" font="default" size="100%">Scoccimarro,E.</style></author><author><style face="normal" font="default" size="100%">Gualdi,S.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Atlantic influence on spring snowfall over the Alps in the past 150 years</style></title><secondary-title><style face="normal" font="default" size="100%">Environmental Research Letters</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Alpine region</style></keyword><keyword><style  face="normal" font="default" size="100%">Atlantic Multi-decadal Oscillation</style></keyword><keyword><style  face="normal" font="default" size="100%">low-frequency climate variability</style></keyword><keyword><style  face="normal" font="default" size="100%">snowfall</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://iopscience.iop.org/1748-9326/8/3/034026/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">8</style></volume><pages><style face="normal" font="default" size="100%">1-8</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Global warming is believed to be responsible for the reduction of snow amount and duration over the Alps. In fact, a rapid shortening of the snowy season has been measured and perceived by ecosystems and society in the past 30 years, despite the large year-to-year variability. This trend is projected to continue during the 21st century in the climate change scenarios with increasing greenhouse gas concentrations. Superimposed on the long-term trend, however, there is a low-frequency variability of snowfall associated with multi-decadal changes in the large-scale circulation. The amplitude of this natural low-frequency variation might be relatively large, determining rapid and substantial changes of snowfall, as recently observed. This is already known for winter snowfall over the Alps in connection with the recent tendency toward the positive phase of the North Atlantic Oscillation. In this study, we show that the low-frequency variability of Alpine spring snowfall in the past 150 years is affected by the Atlantic Multi-decadal Oscillation (AMO), which is a natural periodic fluctuation of Northern Atlantic sea surface temperature. Therefore, the recently observed spring snowfall reduction might be, at least in part, explained by the shift toward a positive AMO phase that happened in the 1990s.</style></abstract></record></records></xml>