Garis salju: Perbedaan antara revisi

[[Berkas:Brunegghorn and Weisshorn.jpg|thumbjmpl|rightka|300px|Gunung [[Weisshorn]]]]

Istilah '''garis salju''' terdiri dari dua pengertian. Pengertian pertama disebut "garis salju klimatikiklim", yaitu batas antara permukaan yang dilapisi oleh [[salju]] dengan permukaan yang bebas salju. Garis salju klimatikiklim dapat berubah-ubah tergantung pada musimnyamusim. Sementara itu, pengertian yang kedua adalah garis salju permanen, yaitu ketinggian tertentu yang saljunya tidak pernah cair pada musim panas atau musim kemarau.

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* Kalesnik, S.V. (1939). Obshchaya glyatsiologiya [General glaciology]. Uchpedgiz, Leningrad, 328 pp. (in Russian)

* Tronov, M.V. (1956). Voprosy svyazi mezhdu klimatom i oledeneniem [The problems of the connection between climate and glaciation]. Izdatel'stvo Tomskogo Universiteta, Tomsk, 202 pp. (in Russian)

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* Braithewaite, R.J. and Raper, S.C.B (2009). "Estimating Equilibrium Line Altitude (ELA) From Glacier Inventory Data." ''Annals of Glaciology'', 50, pp. 127–132. {{doi|10.3189/172756410790595930}}.

* Leonard, K.C., and Fountain, A.G. (2003). "Map-Based Methods for Estimating Glacier Equilibrium-Line Altitudes." ''Journal of Glaciology'', vol. 49, no. 166, pp. 329–336., {{doi|10.3189/172756503781830665}}.

* Ohmura, A., Kasser, P., and Funk, M. (1992). "Climate at the Equilibrium Line of Glaciers." ''Journal of Glaciology'', vol. 38, no. 130, pp. 397–411., {{doi|10.3189/S0022143000002276}}.

* Carrivick, J.L., Lee, J. and Brewer, T.R. (2004). "Improving Local Estimations and Regional Trends of Glacier Equilibrium Line Altitudes." ''Geografiska Annaler. Series A, Physical Geography'', vol. 86, no. 1, pp. 67–79. {{JSTOR|3566202}}.

* Benn, D.I., and Lehmkuhl, F. (2000). "Mass balance and equilibrium-line altitudes of glaciers in high-mountain environments." ''Quaternary International'', 65/66, pp. 15–29. {{doi|10.1016/S1040-6182(99)00034-8}}