Glaciarium continentale

Despectus in Antarcticam e satellite artificiali. Imago composita.

Glaciarium continentale,[1][2] fortasse etiam lamina glaciei,[1][3] in glaciologia est massa glaciei glacialis quae terras circumdatas tegit et aream geometricam plus 50 000 chiliometrorum quadratorum habet.[4] Sola glaciaria continentalia exstantia in Antarctica et Groenlandia inveniuntur; nihilominus, Ultimo Maximo Glaciali temporis glacialis recentissimi, Glaciarium Continentale Laurentidum multum Americae Septentrionalis, glaciarium continentale Weichselianum Europam Septentrionalem, et Glaciarium Continentale Patagonianum australes Americae Australis regiones texerunt.

Notae

  1. ↑ 1.0 1.1 Fons nominis Latini desideratur (addito fonte, hanc formulam remove)
  2. ↑ Anglice continental glacier, "Glossary of Meteorology," American Meteorological Society Formula:Webarchive.
  3. ↑ Anglice ice sheet. In variis linguis (inter quas Francogallica et Hispanica) inlandsis. Theodisce Eisschild, et cetera.
  4. ↑ ""Glossary of Important Terms in Glacial Geology"" .

Bibliographia

  • Müller, Jonas, et Luka Koch. 2012. Ice Sheets: Dynamics, Formation and Environmental Concerns. Hauppauge Novi Eboraci: Nova Science. ISBN 978-1-61942-367-1.
  • Stieg, Eric J., David P. Schneider, Scott Rutherford, Michael E. E. Mann, Josefino C. Comiso, et D. T. Shindell. 2009. "Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year." Nature 457 (7228): 459–62. Bibcode:2009Natur.457..459S. doi:10.1038/nature07669. PMID 19158794. S2CID 4410477. Editio interretialis.
  • Wadham, J. L., J. R. Hawkings, L. Tarasov, L. J. Gregoire, R. G. M. Spencer, M. Gutjahr, A. Ridgwell, et K. E. Kohfeld. 2019. "Ice sheets matter for the global carbon cycle." Nature Communications 10, no. 1 (15 Augusti): 1–17. doi:10.1038/s41467-019-11394-4.

Nexus externi