Earth Insolation and Tendencies of the Variation of Alpine Ice Resources

On the basis of high-precision astronomical ephemeris with a high spatial and temporal resolution, the insolation of the Earth at the upper boundary of the atmosphere was calculated for the period from 3000 BC to 2999 AD. The differences from the earlier calculations of insolation are associated wit...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Geography and natural resources 2021-12, Vol.42 (4), p.297-305
Hauptverfasser:	Fedorov, V. M., Grebennikov, P. B., Frolov, D. M.
Format:	Artikel
Sprache:	eng
Schlagworte:	Algorithms Atmosphere Correlation analysis Earth and Environmental Science Earth surface Economic Geography Equinoxes Frequency variation Geography Glaciation Glaciers Glaciology Heat transfer Insolation Landscape/Regional and Urban Planning Mass balance Northern Hemisphere Regression models Solstices Summer Temporal resolution Winter
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!