Современные климатические изменения, зарегистрированные в вариациях температуры верхнего 80-метрового слоя ледниковой толщи на станции Восток / В.Я. Липенков, Ю.А. Шибаев, А.Н. Саламатин, А.А. Экайкин, Р.Н. Вострецов, А.В. Преображенская.

MARCXML

LDR 03853naa#a2200000#a#4500
001 SPRI-173406
005 20231210102911.0
007 ta
008 231210s2004####xx#a##|##|###|0||#0|rus#d
035 ## ‡aSPRI-173406
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
242 00 ‡aCurrent climate changes recorded in ice temperature variations in upper 80-m layer, Vostok station area.‡yeng
245 00 ‡6880-01‡aSovremennye klimaticheskie izmenenii︠a︡, zaregistrirovannye v variat︠s︡ii︠a︡kh temperatury verkhnego 80-metrovogo sloi︠a︡ lednikovoĭ tolshchi na stant︠s︡ii Vostok /‡cV.I︠A︡. Lipenkov, I︠U︡.A. Shibaev, A.N. Salamatin, A.A. Ėkaĭkin, R.N. Vostret︠s︡ov, A.V. Preobrazhenskai︠a︡.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2004.
300 ## ‡ap. 44-56 :‡bdiags.
500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 97 :44-56 (2004).
500 ## ‡aEnglish summary and figure captions.
520 3# ‡aExamines local short-term temperature changes reflected in uppermost sections of Vostok boreholes. Selects 16 temperature profiles measured between 1961 and 1990 in four dry holes within 100 m of each other. Changes in upper 80 metres imply significant surface temperature increase between 1960 and 1970. Analyses temperature transients over 30 years using heat-transfer model incorporating temperature and density dependent thermal properties of moving firn and ice. Tunes with observations from 1979. Converts isotope record into 200-year surface temperature history. Confirms strong signal that suggests much greater changes in effective driving temperature (+6°C) than in near-surface air temperature (+1°C). Proposes significant difference between isotopic compositions of precipitation and deposited snow due to post-deposition changes controlled by solar radiation.
546 ## ‡aIn Russian.
546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.321.4 -- Temperature, measurement of snow, ice and glaciers.‡2udc
650 07 ‡a551.324.412 -- Land ice, temperature.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a536 -- Heat.‡2udc
650 07 ‡a536.5 -- Temperature measurement and control.‡2udc
650 07 ‡a536.2 -- Heat, transmission.‡2udc
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡a551.582 -- Climatology of particular places.‡2udc
650 07 ‡a551.578.463 -- Snow cover, firnification.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.524 -- Air temperature.‡2udc
650 07 ‡a551.521 -- Radiation, atmospheric.‡2udc
650 07 ‡a551.506 -- Meteorological data.‡2udc
650 07 ‡a551.578.4 -- Ice needles, sleet, falling snow and graupel.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*747.5) -- Vostok region.‡2udc
700 1# ‡6880-02‡aLipenkov, V. I︠A︡.
700 1# ‡6880-03‡aShibaev, I︠U︡. A.
700 1# ‡6880-04‡aSalamatin, A. N.
700 1# ‡6880-05‡aĖkaĭkin, A. A.
700 1# ‡6880-06‡aVostret︠s︡ov, R. N.
700 1# ‡6880-07‡aPreobrazhenskai︠a︡, A. V.
773 0# ‡6880-08‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 97 (2004) ‡wSPRI-33585
880 00 ‡6245-01/(N‡aСовременные климатические изменения, зарегистрированные в вариациях температуры верхнего 80-метрового слоя ледниковой толщи на станции Восток /‡cВ.Я. Липенков, Ю.А. Шибаев, А.Н. Саламатин, А.А. Экайкин, Р.Н. Вострецов, А.В. Преображенская.
880 1# ‡6700-02/(N‡aЛипенков, В. Я.
880 1# ‡6700-03/(N‡aШибаев, Ю. А.
880 1# ‡6700-04/(N‡aСаламатин, А. Н.
880 1# ‡6700-05/(N‡aЭкайкин, А. А.
880 1# ‡6700-06/(N‡aВострецов, Р. Н.
880 1# ‡6700-07/(N‡aПреображенская, А. В.
880 0# ‡6773-08/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 97 (2004) ‡wSPRI-33585
916 ## ‡a2005/10/18 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231210 ‡bRF