Quantum redactiones paginae "Cryosphaera" differant

Content deleted Content added
EmausBot (disputatio | conlationes)
m Bot 1 nexus intervici removet, quod nunc apud Vicidata cum tessera d:Q493109 sunt
m Typo: Vsaintoniae→Vasintoniae &c (10K)
Linea 1:
[[Fasciculus:Cryosphere Fuller Projection.png|thumb|upright=1.2|Conspectus cryosphaerae et eius maiorum elementorum, ex [https://web.archive.org/web/20070826211613/http://maps.grida.no/go/graphic/cryosphere "UN Environment Programme Global Outlook for Ice and Snow"].]]
[[Fasciculus:Components of the Cryosphere.tif|thumb|upright=1.3|[[Regio]]nes ab elementis cryosphaericis in [[orbis terrarum|orbe terrarum]] affectae, ex ''IPCC Fifth Assessment Report.'']]
[[Fasciculus:1249 Finsteraarhorn.jpg|thumb|[[Glaciarium|Glaciaria]] in [[tabula geographica|tabula]] [[topographia|topographica]] repraesentata.]]
'''Cryosphaera''' ([[Graece]] κρύος 'frigor, [[pruina]], [[gelu]]' + σφαῖρα '[[globus]]'<ref>[https://www.perseus.tufts.edu/hopper/text?doc=Perseus%3Atext%3A1999.04.0057%3Aentry%3Dsfai%3Dra^ σφαῖρα], Henry George Liddell et Robert Scott, ''A Greek-English Lexicon,'' apud Perseum.</ref>) est illae [[superficies|superficiei]] [[tellus|telluris]] [[regio]]nes ubi [[aqua]] forma [[solidum|solida]] fit, inter quas [[glacies marina]]e, [[glacies]] [[lacus|lacustrina]]e, glacies [[fluvius|fluviales]], [[nix]], [[glaciarium|glaciaria]], [[glaciarium continentale|glaciaria continentalis]], [[caput glaciei|capita glaciei]], et [[humus]] conglaciatus ([[glacies perpetua|glacie perpetua]] non exclusa). Ergo, cryosphaera multum cum [[hydrosphaera]] congruit. Cryosphaera est necessaria systematis [[clima globale|climatis globalis]] pars, cui sunt coniunctiones et [[retroactio]] per eius momentum in [[energia]] superficiali et [[fluxus|fluxibus]] umidis, [[nubes|nubibus]], [[praecipitatio]]ne, [[hydrologia]], et circulatione [[atmosphaera|atmosphaerica]] [[oceanus|oceanicaque]] effecta. Per quas [[ratio]]nes retroactionis, partes magni momenti agit in climate[[clima]]te globali et in responsis [[exemplar climaticum|exemplaris climatici]] mutationibus globalibus effectis. Regressus [[proprietas|proprietatum]] cryosphaericarum est [[deglaciatio]]; studium cryosphaerarum est [[cryologia]].
 
== Structura ==
Linea 46:
* Martin, S., K. Steffen, J. Comiso, D. Cavalieri, M. R. Drinkwater, et B. Holt. [[1992]]. "Microwave remote sensing of polynyas." In ''Microwave remote sensing of sea ice,'' ed. F. D. Carsey, 303–311. Vasintoniae: American Geophysical Union.
* Meier, M. F. [[1984]]. "Contribution of small glaciers to global sea level rise." ''Science'' 226: 1418–21.
* Parkinson, C. L., J. C. Comiso, H. J. Zwally, D. J. Cavalieri, P. Gloersen, et W. J. Campbell. [[1987]]. ''Arctic Sea Ice, 1973–1976: Satellite Passive-Microwave Observations, NASA SP-489.'' VsaintoniaeVasintoniae: National Aeronautics and Space Administration.
* Paterson, W. S. B. [[1993]]. "World sea level and the present mass balance of the Antarctic ice sheet." In ''Ice in the Climate System,'' ed. W. R. Peltier, 131–40. NATO ASI Series, I12. Berolini: Springer-Verlag.
* Robinson, D. A., K. F. Dewey, et R. R. Heim. [[1993]]. "Global snow cover monitoring: an update." ''Bulletin of the American Meteorolical Sociert'' 74: 1689–96.
Linea 66:
 
[[Categoria:Cryosphaera| ]]
 
{{Myrias|Physica}}