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Jakob Schw
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Jakob Schw
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Jakob Schw
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1
What was the surface temperature in central Antarctica during the last glacial maximum?
by
Thomas Blunier A
,
Jakob
Schw
,
Er A
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2
Change in CO2 concentration and O2/N2 ratio in ice cores due to molecular diffusion
by
Bernhard Bereiter
,
Jakob
Schw
,
Thomas F. Stocker
,
T. F. Stocker
,
Change In Co Concentration
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3
High-resolution Holocene N 2 O ice core record and its relationship
by
With Ch And
,
Jacqueline Flückiger
,
Eric Monnin
,
Bernhard Stauffer
,
Jakob
Schw
,
Thomas F. Stocker
,
Dominique Raynaud
,
Jean-marc Barnola
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4
Title not available
by
Amaelle L
,
Ais Æ Valérie Masson-delmotte
,
Jean Jouzel
,
Æ Dominique Raynaud
,
Æ Sigfus Johnsen
,
Christof Huber
,
Æ Markus Leuenberger
,
Jakob
Schw
,
Er Æ Bénédicte Minster
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5
Palaeogeography, Palaeoclimatology, Palaeoecology 159 (2000) 313--347
by
Www Elsevier Nl
,
Brigitta Ammanna
,
H. J. B. Birks B
,
Stephen J. Brooksd
,
Ulrich Eichere
,
Ulrich Von Grafenstein F
,
Wolfgang Hofmann G
,
Geoffrey Lemdahl H
,
Jakob
Schw
,
Kazimierz Tobolski I
,
Lucia Wick A
Published 2000
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Related Subjects
Antarctic temperature
CH4
CO2
Holocene
N2O
gas occlusion
greenhouse gases
ice core
last glacial maximum
nitrous oxide
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