scholarly article | Q13442814 |
P356 | DOI | 10.1038/NGEO442 |
P50 | author | Hubertus Fischer | Q43271773 |
P2093 | author name string | E. W. Wolff | |
R. Röthlisberger | |||
P2860 | cites work | One-to-one coupling of glacial climate variability in Greenland and Antarctica | Q47292929 |
Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles | Q47297323 | ||
A northern lead in the orbital band: north–south phasing of Ice-Age events | Q54104118 | ||
Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica | Q55880358 | ||
A minimum thermodynamic model for the bipolar seesaw | Q56431763 | ||
Lack of bipolar see-saw in response to Southern Ocean wind reduction | Q57143201 | ||
Ice core evidence for the extent of past atmospheric CO2change due to iron fertilisation | Q58114005 | ||
Reconstruction of millennial changes in dust emission, transport and regional sea ice coverage using the deep EPICA ice cores from the Atlantic and Indian Ocean sector of Antarctica | Q58320828 | ||
Four climate cycles of recurring deep and surface water destabilizations on the Iberian margin | Q80480034 | ||
Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years | Q28241701 | ||
Variations in the Earth's Orbit: Pacemaker of the Ice Ages | Q28245451 | ||
High-resolution carbon dioxide concentration record 650,000-800,000 years before present | Q28280161 | ||
Stable carbon cycle-climate relationship during the Late Pleistocene | Q28283869 | ||
Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period | Q30623431 | ||
The role of the thermohaline circulation in abrupt climate change | Q30675841 | ||
Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation | Q30815410 | ||
Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years | Q31155450 | ||
Atmospheric CO2 concentrations over the last glacial termination | Q33930236 | ||
High-resolution record of Northern Hemisphere climate extending into the last interglacial period | Q34346930 | ||
Orbital and millennial Antarctic climate variability over the past 800,000 years. | Q34646794 | ||
P433 | issue | 3 | |
P407 | language of work or name | English | Q1860 |
P304 | page(s) | 206-209 | |
P577 | publication date | 2009-02-22 | |
P1433 | published in | Nature Geoscience | Q1337483 |
P1476 | title | Glacial terminations as southern warmings without northern control | |
P478 | volume | 2 |
Q34014365 | 800,000 years of abrupt climate variability |
Q58413628 | Anatomy of Heinrich Layer 1 and its role in the last deglaciation |
Q56340173 | Antarctic and global climate history viewed from ice cores |
Q83822933 | Climate change: A tale of two hemispheres |
Q58630564 | Deciphering the spatio-temporal complexity of climate change of the last deglaciation: a model analysis |
Q24289401 | EPICA Dome C record of glacial and interglacial intensities |
Q40510591 | Early warning of climate tipping points from critical slowing down: comparing methods to improve robustness. |
Q58053617 | Evolution of the stable carbon isotope composition of atmospheric CO2over the last glacial cycle |
Q57086702 | Forcing of late Pleistocene ice volume by spatially variable summer energy |
Q39456347 | Holocene Southern Ocean surface temperature variability west of the Antarctic Peninsula. |
Q55919190 | Interglacials of the last 800,000 years |
Q56533757 | Laurentide ice-sheet instability during the last deglaciation |
Q39395630 | Paleoclimate. Enhanced tropical methane production in response to iceberg discharge in the North Atlantic |
Q56100317 | Paleoclimates: what do we learn from deep ice cores? |
Q58878252 | Sea-surface temperature records of Termination 1 in the Gulf of California: Challenges for seasonal and interannual analogues of tropical Pacific climate change |
Q37240120 | Strong coupling of Asian Monsoon and Antarctic climates on sub-orbital timescales |
Q31111358 | The Asian monsoon over the past 640,000 years and ice age terminations |
Q64168372 | The Lower Danube Loess, New Age Constraints from Luminescence Dating, Magnetic Proxies and Isochronous Tephra Markers |
Q34060571 | The early rise and late demise of New Zealand's last glacial maximum |
Q58079221 | The last glacial cycle: transient simulations with an AOGCM |
Q58392099 | Timing of the descent into the last Ice Age determined by the bipolar seesaw |
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