Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2. - Test2 - elhamkhani - TriplyDB

Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

http://www.wikidata.org/entity/Q43529736

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Punctuated Shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 Late-glacial elevated dust deposition linked to westerly wind shifts in southern South America Larger CO₂ source at the equatorial Pacific during the last deglaciation A Southern Ocean trigger for Northwest Pacific ventilation during the Holocene?Hydrologic impacts of past shifts of Earth's thermal equator offer insight into those to be produced by fossil fuel CO2 Global climate evolution during the last deglaciation Deep carbon export from a Southern Ocean iron-fertilized diatom bloom Millennial-scale variability in Antarctic ice-sheet discharge during the last deglaciation Antarctic lakes suggest millennial reorganizations of Southern Hemisphere atmospheric and oceanic circulation Palaeoceanography: motivations and challenges for the future.Rapid interhemispheric climate links via the Australasian monsoon during the last deglaciation.Siple Dome ice reveals two modes of millennial CO2 change during the last ice age.A stagnation event in the deep South Atlantic during the last interglacial period.The influence of historical climate changes on Southern Ocean marine predator populations: a comparative analysis.Proliferation of East Antarctic Adélie penguins in response to historical deglaciation.Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age.Contrasting responses to a climate regime change by sympatric, ice-dependent predators.Ocean dynamics, not dust, have controlled equatorial Pacific productivity over the past 500,000 years.Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes.North Atlantic ocean circulation and abrupt climate change during the last glaciation.Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination The last glacial termination.Climate change. The ice age carbon puzzle.Abrupt change of Antarctic moisture origin at the end of Termination II.Perspectives on empirical approaches for ocean color remote sensing of chlorophyll in a changing climate Antarctic sea ice control on ocean circulation in present and glacial climates Nonlinear climatic sensitivity to greenhouse gases over past 4 glacial/interglacial cycles 800,000 years of abrupt climate variability.Carbon isotope constraints on the deglacial CO₂ rise from ice cores.Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.Detecting ozone- and greenhouse gas-driven wind trends with observational data.Eastern equatorial pacific productivity and related-CO2 changes since the last glacial period.Too much of a good thing: sea ice extent may have forced emperor penguins into refugia during the last glacial maximum.Increased reservoir ages and poorly ventilated deep waters inferred in the glacial Eastern Equatorial Pacific Mode change of millennial CO2 variability during the last glacial cycle associated with a bipolar marine carbon seesaw The Growth Response of Two Diatom Species to Atmospheric Dust from the Last Glacial Maximum.The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sink Glacial reduction and millennial-scale variations in Drake Passage throughflow Human-induced changes in the distribution of rainfall.Large deglacial shifts of the Pacific Intertropical Convergence Zone.

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P2860

Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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2009 nî lūn-bûn

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2009年の論文

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2009年学术文章

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2009年学术文章

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2009年学术文章

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2009年学术文章

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2009年学术文章

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2009年學術文章

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2009年學術文章

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

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B E Anderson

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L H Burckle

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L I Bradtmiller

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M Q Fleisher

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R F Anderson

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S H H Nielsen

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P2860

Interpretation of recent Southern Hemisphere climate change

Eight glacial cycles from an Antarctic ice core

Stable carbon cycle-climate relationship during the Late Pleistocene

Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period.

High-latitude controls of thermocline nutrients and low latitude biological productivity.

Saturation of the southern ocean CO2 sink due to recent climate change.

Comment on "Saturation of the southern ocean CO2 sink due to recent climate change".

Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies.

Atmospheric CO2 and climate on millennial time scales during the last glacial period.

A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization.

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