<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Doveri, Marco</style></author><author><style face="normal" font="default" size="100%">Piccini, Leonardo</style></author><author><style face="normal" font="default" size="100%">Menichini, Matia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrodynamic and Geochemical Features of Metamorphic Carbonate Aquifers and Implications for Water Management: The Apuan Alps (NW Tuscany, Italy) Case Study</style></title><secondary-title><style face="normal" font="default" size="100%">Karst Water Environment </style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Groundwater vulnerability</style></keyword><keyword><style  face="normal" font="default" size="100%">Karst springs</style></keyword><keyword><style  face="normal" font="default" size="100%">Metamorphosed carbonate aquifer</style></keyword><keyword><style  face="normal" font="default" size="100%">Preferential groundwater flow paths</style></keyword><keyword><style  face="normal" font="default" size="100%">Water isotopes</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><number><style face="normal" font="default" size="100%">The Handbook of Environmental Chemistry</style></number><edition><style face="normal" font="default" size="100%">Younos T., Schreiber M., Kosič Ficco K. (eds) Springer</style></edition><volume><style face="normal" font="default" size="100%">68</style></volume><isbn><style face="normal" font="default" size="100%">978-3-319-77367-4</style></isbn><language><style face="normal" font="default" size="100%">eng</style></language><section><style face="normal" font="default" size="100%">Hydrodynamic and Geochemical Features of Metamorphic Carbonate Aquifers and Implications for Water Management: The Apuan Alps (N</style></section></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. Leonelli</style></author><author><style face="normal" font="default" size="100%">G. Battipaglia</style></author><author><style face="normal" font="default" size="100%">P. Cherubini</style></author><author><style face="normal" font="default" size="100%">M. Saurer</style></author><author><style face="normal" font="default" size="100%">R.T.W. Siegwolf</style></author><author><style face="normal" font="default" size="100%">M. Maugeri</style></author><author><style face="normal" font="default" size="100%">B. Stenni</style></author><author><style face="normal" font="default" size="100%">M.L. Fumagalli</style></author><author><style face="normal" font="default" size="100%">M. Pelfini</style></author><author><style face="normal" font="default" size="100%">V. Maggi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Tree-ring δ18O from an Alpine catchment reveals changes in glacier stream water inputs between 1980 and 2010</style></title><secondary-title><style face="normal" font="default" size="100%">ARCTIC, ANTARCTIC, AND ALPINE RESEARCH</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">European larch</style></keyword><keyword><style  face="normal" font="default" size="100%">Forni Glacier</style></keyword><keyword><style  face="normal" font="default" size="100%">glacier meltwater</style></keyword><keyword><style  face="normal" font="default" size="100%">Tree-ring stable isotopes</style></keyword><keyword><style  face="normal" font="default" size="100%">water stable isotopes</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1080/15230430.2019.1623607</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">51</style></volume><pages><style face="normal" font="default" size="100%">250–264</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%">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%">Toreti, A</style></author><author><style face="normal" font="default" size="100%">Schindler, A</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 multi-decadal oscillation influence on weather regimes over Europe and the Mediterranean in spring and summer</style></title><secondary-title><style face="normal" font="default" size="100%">Global and Planetary Change</style></secondary-title><short-title><style face="normal" font="default" size="100%">Glob. Planet. Change</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">20th century reanalysis</style></keyword><keyword><style  face="normal" font="default" size="100%">Atmospheric circulation</style></keyword><keyword><style  face="normal" font="default" size="100%">Decadal variability</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean climate</style></keyword><keyword><style  face="normal" font="default" size="100%">Weather regimes</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1016/j.gloplacha.2016.08.014</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%">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></records></xml>