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Record #156364:
- #156364
Main publication details
MARC recordClimate change and palaeoceanography / Morten Hald.
| Title: | Climate change and palaeoceanography / Morten Hald. |
| Author(s): | Hald, Morten. |
| Date: | 2000. |
| Publisher: | Heidelberg, Germany: Springer |
| In: | Northern North Atlantic : a changing environment. (2000.), |
| Abstract: | Reviews palaeoclimatic evolution during last interglacial-glacial cycle in Norwegian-Greenland Seas as reconstructed from sediment studies. These seas have long been very sensitive to climatic changes. Initial response to orbitally forced change occurs at high latitudes. With Norwegian, West Spitsbergen and Irminger Currents, large amounts of heat are released into atmosphere when water sinks to become North Atlantic Deep Water, which also acts as sink for atmospheric CO₂, ventilating large part of deep waters of world ocean. Climate phases in last 500 000 years and early marine geological investigations are described. |
| Notes: | In: The northern North Atlantic : a changing environment / Priska Schäfer, Will Ritzrau, Michael Schlüter, Jörn Thiede, eds. |
| Keywords: | 551.3.051 -- Sedimentation and stratification. 551.465 -- Oceanography, dynamics. 551.583.3 -- Climatic changes, Quaternary. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*61) -- North Atlantic Ocean. (*615) -- Norwegian Sea. (*617) -- Greenland Sea and Fram Strait. |
| SPRI record no.: | 156364 |
LDR 01804naa#a2200000#a#4500 001 SPRI-156364 005 20240418110354.0 007 ta 008 240418s2000####gw#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-156364 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHald, Morten. 245 10 ‡aClimate change and palaeoceanography /‡cMorten Hald. 260 ## ‡aHeidelberg, Germany :‡bSpringer,‡c2000. 300 ## ‡ap. 281-290 :‡bdiags., map. 500 ## ‡aIn: The northern North Atlantic : a changing environment / Priska Schäfer, Will Ritzrau, Michael Schlüter, Jörn Thiede, eds. 520 3# ‡aReviews palaeoclimatic evolution during last interglacial-glacial cycle in Norwegian-Greenland Seas as reconstructed from sediment studies. These seas have long been very sensitive to climatic changes. Initial response to orbitally forced change occurs at high latitudes. With Norwegian, West Spitsbergen and Irminger Currents, large amounts of heat are released into atmosphere when water sinks to become North Atlantic Deep Water, which also acts as sink for atmospheric CO₂, ventilating large part of deep waters of world ocean. Climate phases in last 500 000 years and early marine geological investigations are described. 650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc 650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡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(*615) -- Norwegian Sea.‡2udc 651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc 773 0# ‡7nnam ‡aPriska Schäfer, Will Ritzrau, Michael Schlüter, Jörn Thiede, eds. ‡tNorthern North Atlantic : a changing environment. ‡dHeidelberg, Germany : Springer, 2000. ‡wSPRI-154853 876 ## ‡jMissing 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418 ‡dMISSING[2004]