Eric J Steig
Biographic Data
| ID | 5646325 |
|---|---|
| NAME | Eric J Steig |
| GIVEN NAMES | Eric J |
| FAMILY NAME | Steig |
| SIGNATURE | STEIG E J |
| AFFILIATIONS | University of Washington |
| ORCID | 0000-0002-8191-5549 |
| VERIFIED | Yes |
| TOTAL WORKS | 10 |
| TOTAL CITATIONS | 6 |
| AUTHOR COUNT | 10 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2000 |
| LATEST PUBLICATION YEAR | 2014 |
| H-INDEX | 1 |
Ice Cores from the St. Elias Mountains, Yukon, Canada
A major achievement in research supported by the Kluane Lake Research Station was the recovery, in 2001 – 02, of a suite of cores from the icefields of the central St. Elias Mountains, Yukon, by teams of researchers from Canada, the United States, and Japan. This project led to the development of parallel, long (103 – 104 year) ice-core records of climate and atmospheric change over an altitudinal range of more than 2 km, from the Eclipse Icefiel…
Continental-scale temperature variability during the past two millennia
Preliminary results from a new high-resolution ice core from Combatant Col, Mount Waddington, British Columbia, Canada
The Mt Logan Holocene—late Wisconsinan isotope record
The ice core recovered from Prospector Russell Col on Mt Logan (5.4 km a.s.l.), in the Yukon spans over 20 000 years. This unique record offers a Pacific view of the stable isotope and chemical record from the Lateglacial to the present. The timescale is based on seasonal counted years, the largest known volcanic acid signatures and the major shift in stable isotopes and chemistry at the end of the Younger Dryas. There are large and sustained cha…
Another look at An Inconvenient Truth
Holocene Climate and Cultural Evolution in Late Prehistoric–Early Historic West Asia
is the result of the workshop "Paleoclimate Proxy Data for Reconstructing Holocene Environments of West Asia" held at the 4th International Congress on the Archaeology of the Ancient Near East in Berlin, March 20 to April 3, 2004. The objective of the workshop was to gather scientists from the usually separate archaeological and geoscience communities to stimulate discussion in the interdisciplinary field of climate change in late prehistoricearl…
Holocene thermal maximum in the western Arctic (0–180°W)
Holocene climate variability
Although the dramatic climate disruptions of the last glacial period have received considerable attention, relatively little has been directed toward climate variability in the Holocene (11,500 cal yr B.P. to the present). Examination of ?50 globally distributed paleoclimate records reveals as many as six periods of significant rapid climate change during the time periods 9000"8000, 6000"5000, 4200"3800, 3500"2500, 1200"1000, and 600"150 cal yr B…
The Taylor Dome Antarctic 18 O Record and Globally Synchronous Changes in Climate
The 18 O/ 16 O profile of a 554-m long ice core through Taylor Dome, Antarctica, shows the climate variability of the last glacial–interglacial cycle in detail and extends at least another full cycle. Taylor Dome shares the main features of the Vostok record, including the early climatic optimum with later cool phase of the last interglacial period in Antarctica. Taylor Dome δ 18 O fluctuations are more abrupt and larger than those at Vostok and …
Holocene Climate Variability in Antarctica Based on 11 Ice-Core Isotopic Records
A comparison is made of the Holocene records obtained from water isotope measurements along 11 ice cores from coastal and central sites in east Antarctica (Vostok, Dome B, Plateau Remote, Komsomolskaia, Dome C, Taylor Dome, Dominion Range, D47, KM105, and Law Dome) and west Antarctica (Byrd), with temporal resolution from 20 to 50 yr. The long-term trends possibly reflect local ice sheet elevation fluctuations superimposed on common climatic fluc…
The Mt Logan Holocene—late Wisconsinan isotope record
The ice core recovered from Prospector Russell Col on Mt Logan (5.4 km a.s.l.), in the Yukon spans over 20 000 years. This unique record offers a Pacific view of the stable isotope and chemical record from the Lateglacial to the present. The timescale is based on seasonal counted years, the largest known volcanic acid signatures and the major shift in stable isotopes and chemistry at the end of the Younger Dryas. There are large and sustained cha…
Holocene Climate Variability in Antarctica Based on 11 Ice-Core Isotopic Records
A comparison is made of the Holocene records obtained from water isotope measurements along 11 ice cores from coastal and central sites in east Antarctica (Vostok, Dome B, Plateau Remote, Komsomolskaia, Dome C, Taylor Dome, Dominion Range, D47, KM105, and Law Dome) and west Antarctica (Byrd), with temporal resolution from 20 to 50 yr. The long-term trends possibly reflect local ice sheet elevation fluctuations superimposed on common climatic fluc…
The Taylor Dome Antarctic 18 O Record and Globally Synchronous Changes in Climate
The 18 O/ 16 O profile of a 554-m long ice core through Taylor Dome, Antarctica, shows the climate variability of the last glacial–interglacial cycle in detail and extends at least another full cycle. Taylor Dome shares the main features of the Vostok record, including the early climatic optimum with later cool phase of the last interglacial period in Antarctica. Taylor Dome δ 18 O fluctuations are more abrupt and larger than those at Vostok and …
Holocene thermal maximum in the western Arctic (0–180°W)
Holocene climate variability
Although the dramatic climate disruptions of the last glacial period have received considerable attention, relatively little has been directed toward climate variability in the Holocene (11,500 cal yr B.P. to the present). Examination of ?50 globally distributed paleoclimate records reveals as many as six periods of significant rapid climate change during the time periods 9000"8000, 6000"5000, 4200"3800, 3500"2500, 1200"1000, and 600"150 cal yr B…
Holocene Climate and Cultural Evolution in Late Prehistoric–Early Historic West Asia
is the result of the workshop "Paleoclimate Proxy Data for Reconstructing Holocene Environments of West Asia" held at the 4th International Congress on the Archaeology of the Ancient Near East in Berlin, March 20 to April 3, 2004. The objective of the workshop was to gather scientists from the usually separate archaeological and geoscience communities to stimulate discussion in the interdisciplinary field of climate change in late prehistoricearl…
Another look at An Inconvenient Truth
The Mt Logan Holocene—late Wisconsinan isotope record
The ice core recovered from Prospector Russell Col on Mt Logan (5.4 km a.s.l.), in the Yukon spans over 20 000 years. This unique record offers a Pacific view of the stable isotope and chemical record from the Lateglacial to the present. The timescale is based on seasonal counted years, the largest known volcanic acid signatures and the major shift in stable isotopes and chemistry at the end of the Younger Dryas. There are large and sustained cha…
Continental-scale temperature variability during the past two millennia
Preliminary results from a new high-resolution ice core from Combatant Col, Mount Waddington, British Columbia, Canada
Ice Cores from the St. Elias Mountains, Yukon, Canada
A major achievement in research supported by the Kluane Lake Research Station was the recovery, in 2001 – 02, of a suite of cores from the icefields of the central St. Elias Mountains, Yukon, by teams of researchers from Canada, the United States, and Japan. This project led to the development of parallel, long (103 – 104 year) ice-core records of climate and atmospheric change over an altitudinal range of more than 2 km, from the Eclipse Icefiel…
Geography (9 works) · Geology and Paleoclimatology Research (9 works) · Climate change (7 works) · Climatology (7 works) · Geology (7 works) · Physical geography (7 works) · Holocene (6 works) · Oceanography (6 works) · Ice core (5 works) · Paleoclimatology (5 works)