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Record #110151:

Polar ice cores and climate history / David A. Peel.

Title: Polar ice cores and climate history / David A. Peel.
Author(s): Peel, David A.
Date: 1991.
In: Weather. (1991.), Vol. 46(4) (1991)
Abstract: Points out value to studies of present and future climate of ice cores recovered from polar ice sheets. Atmospheric conditions are preserved in ice in three ways: isotopes (principally stable isotopes of oxygen and hydrogen), soluble and insoluble aerosols scavenged by snowfall or deposited on surface by dry deposition (continental dust, sea salts, volcanic shards and acids, extraterrestrial material and traces of industrial pollution), and bubbles of air containing atmospheric gases. From this evidence, past climates can be deduced and events during last glacial cycle can be followed. Cores also give clues on related factors that may have been implicated in changes, either causally or by contributing to positive feedback processes that amplify responses.
Notes:

Weather. Vol. 46(4) :95-102 (1991).

Keywords: 551.324.82 -- Bubbles in glaciers and ice.
551.324.84 -- Land ice, impurities.
551.324 -- Land ice.
54 -- Chemistry.
54.027 -- Isotope analysis.
551.58 -- Climatology.
551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
551.588 -- Climate, effect of man and environment.
551.32 -- Glaciology.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
E5 -- Glaciology: land ice.
(*2) -- Polar regions.
(*7) -- Antarctic regions.
(*38) -- Greenland.
SPRI record no.: 110151

MARCXML

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008 230401s1991####xx#a##|##|###|0||#0|eng#d
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100 1# ‡aPeel, David A.
245 10 ‡aPolar ice cores and climate history /‡cDavid A. Peel.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 95-102 :‡bill., diags.
500 ## ‡aWeather. Vol. 46(4) :95-102 (1991).
520 3# ‡aPoints out value to studies of present and future climate of ice cores recovered from polar ice sheets. Atmospheric conditions are preserved in ice in three ways: isotopes (principally stable isotopes of oxygen and hydrogen), soluble and insoluble aerosols scavenged by snowfall or deposited on surface by dry deposition (continental dust, sea salts, volcanic shards and acids, extraterrestrial material and traces of industrial pollution), and bubbles of air containing atmospheric gases. From this evidence, past climates can be deduced and events during last glacial cycle can be followed. Cores also give clues on related factors that may have been implicated in changes, either causally or by contributing to positive feedback processes that amplify responses.
650 07 ‡a551.324.82 -- Bubbles in glaciers and ice.‡2udc
650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.588 -- Climate, effect of man and environment.‡2udc
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 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*2) -- Polar regions.‡2udc
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
773 0# ‡7nnas ‡tWeather. ‡gVol. 46(4) (1991) ‡wSPRI-20188
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230401