01245nam0-2200373li-450-9900002580402033160025804USA010025804(ALEPH)000025804USA01002580420001109d1968----km-y0itay0103----baengUSLinear and quasilinear elliptic equationsOlga A. Ladyzhenskaya and Nina N. Ural'tsevatranslated by Scripta Tecnicatranslation editor: Leon EhrenpreisNew YorkAcademic Press1968Trad. di: lineynyye kvazilineynyyeuravneniya ellipticheskogo tipaaltro genereequazioni differenziali parzialiequazioni ellittiche515353Equazioni differenziali parzialiLadyzhenskaya,Olga A.Ehrenpreis,LeonUral'ceva Nina N.Scripta TecnicaSistema bibliotecario di Ateneo dell' Universit� di SalernoRICA990000258040203316510 MSE (46)0002873BKSCI1990022020001110USA01171520020403USA011634PATRY9020040406USA011618UNISA04231nam 22010453a 450 991036775950332120250203235437.09783039213245303921324510.3390/books978-3-03921-324-5(CKB)4100000010106122(oapen)https://directory.doabooks.org/handle/20.500.12854/43784(ScCtBLL)131cdb6f-1c59-4ca1-ab03-ddcc7ecf5d61(OCoLC)1163833381(oapen)doab43784(oapen)43784(EXLCZ)99410000001010612220250203i20192019 uu engurmn|---annantxtrdacontentcrdamediacrrdacarrierCondensed Matter Researches in Cryospheric ScienceValter Maggi, Cunde Xiao, Augusto MarcelliMDPI - Multidisciplinary Digital Publishing Institute2019Basel, Switzerland :MDPI,2019.1 electronic resource (144 p.)9783039213238 3039213237 The cryosphere is very sensitive to climate change, and glaciers represent one of the most important archives of atmospheric composition and its variability. From the Himalaya to the European Alps, the longest mid-latitude mountain chain in the world, lie thousands of glaciers that have collected atmospheric compounds over the last millennia. China and Italy are located at the opposite terminals of this long mountain chain, comprising strategic positions for understanding climate evolution and providing important information for the modeling of future climates. The results presented are highlights of some of the most recent advances in cryospheric studies, especially on the topic of mineral dust and aerosols in the atmosphere. They evidence the complexity of the chemical-physical processes involving solid compounds occurring in glacier, snow, and permafrost environments, covering different aspects such as spatial and temporal trends, as well as the impact of mineral and nonmineral particles. Results also show that recent advances in measurement techniques and source apportionment may be powerful and sophisticated tools to provide novel, high-quality scientific information.Environmental economicsbicsscXAS spectroscopybacteriaXANESmineral elementsX-ray fluorescence spectroscopyiron geochemistryiceX-ray absorption fine structure spectroscopymineral dustcompositional data analysissynchrotron radiationdustglobal warming hiatussimultaneous measurementsTXRFlow concentration elemental analysisglobal warming slowdownpaleoclimatologywaterX-ray fluorescencesnowlong-range transportsouthern hemisphereAntarcticaice corecryoconiteevaporationcontaminantsPOPspaleoclimateXANES and LCFultra-dilutionparticulate mattertrace elementsatmospheric mineral dustcryospheric sciencesice coresX-ray absorption near edge spectroscopydropletsArctic rapid warmingmicrobiologycryospherepolycapillary opticsenvironmentLaohugou glacieriron speciationX-ray absorption spectroscopyArcticinsoluble dustEnvironmental economicsMaggi Valter272824Xiao CundeMarcelli A.ScCtBLLScCtBLLBOOK9910367759503321Condensed Matter Researches in Cryospheric Science4318291UNINA