skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #171169:

Deep convection in the Irminger Sea forced by the Greenland tip jet / Robert S. Pickart, Michael A. Spall, Mads Hvid Ribergaard, G.W.K. Moore, Ralph F. Milliff.

Title: Deep convection in the Irminger Sea forced by the Greenland tip jet / Robert S. Pickart, Michael A. Spall, Mads Hvid Ribergaard, G.W.K. Moore, Ralph F. Milliff.
Author(s): Pickart, Robert S.
Spall, Michael A.
Ribergaard, Mads Hvid.
Moore, G. W. K.
Milliff, Ralph F.
Date: 2003.
In: Nature. (2003.), Vol. 424(6945) (2003)
Abstract: Shows that most likely cause of convection is low-level atmospheric jet from lee of Cape Farewell, with high heat flux and strong wind stress curl. Land station data and model show that deep convection can occur when North Atlantic Oscillation is high. Mechanism is significantly different from those in Labrador Sea and Mediterranean.
Notes:

Nature. Vol. 424(6945) :152-156 (2003).

Keywords: 551.465 -- Oceanography, dynamics.
551.465.4 -- Oceanography, stratification.
551.51 -- Atmosphere. Structure, mechanics and thermodynamics.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*61) -- North Atlantic Ocean.
(*617) -- Greenland Sea and Fram Strait.
SPRI record no.: 171169

MARCXML

LDR 01486naa#a2200000#a#4500
001 SPRI-171169
005 20240419003424.0
007 ta
008 240419s2003####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-171169
040 ## ‡aUkCU-P‡beng‡eaacr
245 00 ‡aDeep convection in the Irminger Sea forced by the Greenland tip jet /‡cRobert S. Pickart, Michael A. Spall, Mads Hvid Ribergaard, G.W.K. Moore, Ralph F. Milliff.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 152-156 :‡bdiags., maps.
500 ## ‡aNature. Vol. 424(6945) :152-156 (2003).
520 3# ‡aShows that most likely cause of convection is low-level atmospheric jet from lee of Cape Farewell, with high heat flux and strong wind stress curl. Land station data and model show that deep convection can occur when North Atlantic Oscillation is high. Mechanism is significantly different from those in Labrador Sea and Mediterranean.
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.4 -- Oceanography, stratification.‡2udc
650 07 ‡a551.51 -- Atmosphere. Structure, mechanics and thermodynamics.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
700 1# ‡aPickart, Robert S.
700 1# ‡aSpall, Michael A.
700 1# ‡aRibergaard, Mads Hvid.
700 1# ‡aMoore, G. W. K.
700 1# ‡aMilliff, Ralph F.
773 0# ‡7nnas ‡tNature. ‡gVol. 424(6945) (2003) ‡wSPRI-1046
916 ## ‡a2005/10/18 -- JP
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419 ‡bJP