Arus termohalin

Sirkulasi termohalin adalah sebuah bagian dari sirkulasi samudera berskala besar yang didorong oleh gradien kepadatan global yang dihasilkan oleh panas permukaan dan fluks air tawar.^[1]^[2] Sebutan termohalin berasal dari kata thermo- yang merujuk kepada temperatur dan -haline yang merujuk kepada kandungan garam, faktor-faktor yang sama-sama menentukan kepadatan air laut.

Penjelasan dari wadah sirkulasi termohalin. Wadah biru mewakili arus kedalaman air, sementara wadah merah mewakili arus permukaan.

Referensi

^ Rahmstorf, S (2003). "The concept of the thermohaline circulation" (PDF). Nature. 421 (6924): 699. Bibcode:2003Natur.421..699R. doi:10.1038/421699a. PMID 12610602.
^ Lappo, SS (1984). "On reason of the northward heat advection across the Equator in the South Pacific and Atlantic ocean". Study of Ocean and Atmosphere Interaction Processes. Moscow Department of Gidrometeoizdat (in Mandarin): 125–9.

Sumber lain

Apel, JR (1987). Principles of Ocean Physics. Academic Press. ISBN 0-12-058866-8.
Gnanadesikan, A.; R. D. Slater; P. S. Swathi; G. K. Vallis (2005). "The energetics of ocean heat transport". Journal of Climate. 18 (14): 2604–16. Bibcode:2005JCli...18.2604G. doi:10.1175/JCLI3436.1.
Knauss, JA (1996). Introduction to Physical Oceanography. Prentice Hall. ISBN 0-13-238155-9.
"Potential Impact of Climate Change". United Nations Environment Programme / GRID-Arendal. 2006. Diarsipkan dari versi asli tanggal 2017-01-28. Diakses tanggal 2018-08-20.
Rahmstorf, S (2006). "Thermohaline Ocean Circulation" (PDF). Dalam Elias, S. A. Encyclopedia of Quaternary Sciences. Elsevier Science. ISBN 0-444-52747-8.

Pranala luar

Ocean Conveyor Belt
THOR FP7 projects http://arquivo.pt/wayback/20141126093524/http%3A//www.eu%2Dthor.eu/ investigates on the topic "Thermohaline overturning- at risk?" and the predictability of changes of the THC. THOR is financed by the 7th Framework Programme of the European Commission.

[1] Rahmstorf, S (2003). "The concept of the thermohaline circulation" (PDF). Nature. 421 (6924): 699. Bibcode:2003Natur.421..699R. doi:10.1038/421699a. PMID 12610602.

[2] Lappo, SS (1984). "On reason of the northward heat advection across the Equator in the South Pacific and Atlantic ocean". Study of Ocean and Atmosphere Interaction Processes. Moscow Department of Gidrometeoizdat (in Mandarin): 125–9.

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