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 It is no longer being updated, so does not reliably reflect our current library holdings.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 |
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