<?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%">C. Cerrato</style></author><author><style face="normal" font="default" size="100%">E. Rocchia</style></author><author><style face="normal" font="default" size="100%">M. Brunetti</style></author><author><style face="normal" font="default" size="100%">R. Bionda</style></author><author><style face="normal" font="default" size="100%">B. Bassano</style></author><author><style face="normal" font="default" size="100%">A. Provenzale</style></author><author><style face="normal" font="default" size="100%">S. Bonelli</style></author><author><style face="normal" font="default" size="100%">R. Viterbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Butterfly distribution along altitudinal gradients: temporal changes over a short time period</style></title><secondary-title><style face="normal" font="default" size="100%">Nature Conservation</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Butterfly</style></keyword><keyword><style  face="normal" font="default" size="100%">community composition</style></keyword><keyword><style  face="normal" font="default" size="100%">LTER</style></keyword><keyword><style  face="normal" font="default" size="100%">mountain ecosystem</style></keyword><keyword><style  face="normal" font="default" size="100%">protected area</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">In Press</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://natureconservation.pensoft.net</style></url></web-urls></urls><isbn><style face="normal" font="default" size="100%">1314–6947 </style></isbn><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%">G. Baiamonte</style></author><author><style face="normal" font="default" size="100%">L. Mercalli</style></author><author><style face="normal" font="default" size="100%">D. Cat Merro</style></author><author><style face="normal" font="default" size="100%">C. Agnese</style></author><author><style face="normal" font="default" size="100%">S. Ferraris</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Modelling the frequency distribution of inter-arrival times from daily precipitation time-series in North-West Italy</style></title><secondary-title><style face="normal" font="default" size="100%">Hydrology Research</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">dry spells</style></keyword><keyword><style  face="normal" font="default" size="100%">inter-arrival times</style></keyword><keyword><style  face="normal" font="default" size="100%">Lerch probability distribution</style></keyword><keyword><style  face="normal" font="default" size="100%">rainfall regime</style></keyword><keyword><style  face="normal" font="default" size="100%">water scarcity</style></keyword><keyword><style  face="normal" font="default" size="100%">wet spells</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%">07/2018</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.2166/nh.2018.042 </style></url></web-urls></urls><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>