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Record #104118:
- #104118
Main publication details
MARC record200-hundred year climate record from Antarctic Peninsula (abstract) / David A. Peel, Robert Mulvaney.
| Title: | 200-hundred year climate record from Antarctic Peninsula (abstract) / David A. Peel, Robert Mulvaney. |
| Author(s): | Peel, David A. Mulvaney, Robert. |
| Date: | 1990. |
| In: | Annals of Glaciology. (1990.), Vol. 14 (1990) |
| Abstract: | From previous ice-core studies by these and other authors, it is now possible to propose regional climatic signal for Weddell Sea coastal sector of peninsula. Most striking feature is broad maximum in δ¹⁸O for mid-19th century, implying decadal average temperature at least as high as present, contrasting with evidence from elsewhere in southern hemisphere. Tentative explanations are proposed, based on evidence for period (1974-80) where climatic shifts are clearly amplified in isotopic records. |
| Notes: | Annals of Glaciology. Vol. 14 :353 (1990). |
| Keywords: | 551.32 -- Glaciology. 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc. 622.14 -- Core sampling, ice and snow. 551.324.84 -- Land ice, impurities. 551.324 -- Land ice. 539.155.2 -- Isotopic analysis. 551.583.3 -- Climatic changes, Quaternary. E9 -- Glaciology: meteorology and climatology. (*7) -- Antarctic regions. (*726) -- Maritime Antarctic. (*726.3) -- Antarctic Peninsula. (*726.88) -- Black Coast. |
| SPRI record no.: | 104118 |
LDR 01681naa#a2200000#a#4500 001 SPRI-104118 005 20230324190924.0 007 ta 008 230324s1990####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-104118 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPeel, David A. 245 10 ‡a200-hundred year climate record from Antarctic Peninsula (abstract) /‡cDavid A. Peel, Robert Mulvaney. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 353. 500 ## ‡aAnnals of Glaciology. Vol. 14 :353 (1990). 520 3# ‡aFrom previous ice-core studies by these and other authors, it is now possible to propose regional climatic signal for Weddell Sea coastal sector of peninsula. Most striking feature is broad maximum in δ¹⁸O for mid-19th century, implying decadal average temperature at least as high as present, contrasting with evidence from elsewhere in southern hemisphere. Tentative explanations are proposed, based on evidence for period (1974-80) where climatic shifts are clearly amplified in isotopic records. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc 650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc 650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a539.155.2 -- Isotopic analysis.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*726) -- Maritime Antarctic.‡2udc 651 #7 ‡a(*726.3) -- Antarctic Peninsula.‡2udc 651 #7 ‡a(*726.88) -- Black Coast.‡2udc 700 1# ‡aMulvaney, Robert. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 14 (1990) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230324