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[PDF] Top 20 Antarctic ice-sheet response to atmospheric CO<sub>2</sub> and insolation in the Middle Miocene

Has 10000 "Antarctic ice-sheet response to atmospheric CO<sub>2</sub> and insolation in the Middle Miocene" found on our website. Below are the top 20 most common "Antarctic ice-sheet response to atmospheric CO<sub>2</sub> and insolation in the Middle Miocene".

Antarctic ice-sheet response to atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and insolation in the Middle Miocene

Antarctic ice-sheet response to atmospheric CO<sub>2</sub> and insolation in the Middle Miocene

... The ice-sheet model is symmetric around the South ...Within the ice sheet, flow velocities and temperatures are computed with a vertical resolution of 12 ...layers. ... See full document

14

Tightened constraints on the time-lag between Antarctic temperature and CO&lt;sub&gt;2&lt;/sub&gt; during the last deglaciation

Tightened constraints on the time-lag between Antarctic temperature and CO<sub>2</sub> during the last deglaciation

... while the other supports a greater role for the ocean (Schmittner and Galbraith, 2008; Skinner et ...specifies the proximal trigger of deglacial warming; indeed, this important point is not ... See full document

9

Synergism between elevated &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; and temperature on the Antarctic sea ice diatom &lt;i&gt;Nitzschia lecointei&lt;/i&gt;

Synergism between elevated <i>p</i>CO<sub>2</sub> and temperature on the Antarctic sea ice diatom <i>Nitzschia lecointei</i>

... tion in photosynthesis when CO 2 is limited (see Reinfelder, ...evolutionary response to the change of atmospheric gases over geological time, where the ratio of O ... See full document

33

Atmospheric inversion for cost effective quantification of city CO&lt;sub&gt;2&lt;/sub&gt; emissions

Atmospheric inversion for cost effective quantification of city CO<sub>2</sub> emissions

... T., and Yuen, C.-W.: Towards robust regional estimates of CO 2 sources and sinks using atmospheric transport models, Nature, 415, 626–630, ...B., and Abdul-Massih, ... See full document

64

A global coupled Eulerian-Lagrangian model and 1 × 1 km CO&lt;sub&gt;2&lt;/sub&gt; surface flux dataset for high-resolution atmospheric CO&lt;sub&gt;2&lt;/sub&gt; transport simulations

A global coupled Eulerian-Lagrangian model and 1 × 1 km CO<sub>2</sub> surface flux dataset for high-resolution atmospheric CO<sub>2</sub> transport simulations

... fluxes the number of vegeta- tion types at each grid point (on a ...extended to include all possible types. The fluxes were interpolated spatially to each pixel of the vegetation ... See full document

34

A novel model to predict the physical state of atmospheric H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;/NH&lt;sub&gt;3&lt;/sub&gt;/H&lt;sub&gt;2&lt;/sub&gt;O aerosol particles

A novel model to predict the physical state of atmospheric H<sub>2</sub>SO<sub>4</sub>/NH<sub>3</sub>/H<sub>2</sub>O aerosol particles

... enhance the Earth’s albedo, their direct effect results in a net cool- ...However, the level of confidence in the quantification of this effect is low ( IPCC, 2001) due to ... See full document

39

Sensitivity of simulated CO&lt;sub&gt;2&lt;/sub&gt; concentration to  regridding of global fossil fuel CO&lt;sub&gt;2&lt;/sub&gt; emissions

Sensitivity of simulated CO<sub>2</sub> concentration to regridding of global fossil fuel CO<sub>2</sub> emissions

... 2010). The model uses dynamical fields from the Modern-Era Retrospective anal- ysis for Research and Applications (MERRA) (Bosilovich, 2013), which is a NASA reanalysis for the satellite era ... See full document

8

Error correlation between CO&lt;sub&gt;2&lt;/sub&gt; and CO as constraint for CO&lt;sub&gt;2&lt;/sub&gt; flux inversions using satellite data

Error correlation between CO<sub>2</sub> and CO as constraint for CO<sub>2</sub> flux inversions using satellite data

... of the observational errors are not strictly in- ...ance. The error variances add quadratically (if the errors are ...independent). The instrument error includes measure- ment noise ... See full document

11

Automatic processing of atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; mole fractions at
the ICOS Atmosphere Thematic Centre

Automatic processing of atmospheric CO<sub>2</sub> and CH<sub>4</sub> mole fractions at the ICOS Atmosphere Thematic Centre

... through the whole air inlet, and possible bias due to a con- tamination in the inlet upstream the connection of the target gas is not ...range in the mole ... See full document

18

Ten years of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt;, CO and N&lt;sub&gt;2&lt;/sub&gt;O fluxes over Western Europe inferred from atmospheric measurements at Mace Head, Ireland

Ten years of CO<sub>2</sub>, CH<sub>4</sub>, CO and N<sub>2</sub>O fluxes over Western Europe inferred from atmospheric measurements at Mace Head, Ireland

... for the European region computed using the radon tracer method between 1996 and 2004 ...plotted in black and the NAME transport model results in grey [Manning et ...2003]. ... See full document

47

The influence of the stratosphere on the tropospheric zonal wind response to CO&lt;sub&gt;2&lt;/sub&gt; doubling

The influence of the stratosphere on the tropospheric zonal wind response to CO<sub>2</sub> doubling

... Through the thermal wind relationship, this is related to increased westerly winds in the midlatitudes, in the tropopause region, but with a pos- sible downward influence toward ... See full document

31

Interannual variability of the atmospheric CO&lt;sub&gt;2&lt;/sub&gt; growth rate: roles of  precipitation and temperature

Interannual variability of the atmospheric CO<sub>2</sub> growth rate: roles of precipitation and temperature

... J., and Torres-Lezama, A.: Drought Sensi- tivity of the Amazon Rainforest, Science, 323, 1344–1347, ...S., and Zeng, ...their response to climate variability and to ... See full document

14

Free atmospheric CO&lt;sub&gt;2&lt;/sub&gt; enrichment did not affect symbiotic N&lt;sub&gt;2&lt;/sub&gt;-fixation and soil carbon dynamics in a mixed deciduous stand in Wales

Free atmospheric CO<sub>2</sub> enrichment did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales

... while the soil C/N ratio was not affected by ...Bangor the major mechanism to sustain increased NPP under FACE is also based on increased ...with the conclusions of (Finzi et al., 2007) (Table ... See full document

28

Anthropogenic CO&lt;sub&gt;2&lt;/sub&gt; emissions in Africa

Anthropogenic CO<sub>2</sub> emissions in Africa

... pollution and increased energy efficiency, characteristics to which all nations ...deforestation in Africa were higher than those in tropical Asia and nearly as high as those in ... See full document

17

Comparisons of continuous atmospheric CH&lt;sub&gt;4&lt;/sub&gt;, CO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O measurements &amp;ndash; results from a travelling instrument campaign at Mace Head

Comparisons of continuous atmospheric CH<sub>4</sub>, CO<sub>2</sub> and N<sub>2</sub>O measurements &ndash; results from a travelling instrument campaign at Mace Head

... months and are analysed at Scripps Institute of Oceanography (SIO) before and after use at Mace Head, for details see Prinn et ...with the old working standards and agree well with the ... See full document

16

A model study on the sensitivity of surface ocean CO&lt;sub&gt;2&lt;/sub&gt; pressure with respect to the CO&lt;sub&gt;2&lt;/sub&gt; gas exchange rate

A model study on the sensitivity of surface ocean CO<sub>2</sub> pressure with respect to the CO<sub>2</sub> gas exchange rate

... R., and de Baar, H. J. W.: Climatological mean and decadal change in surface ocean pCO 2 , and net sea-air CO 2 flux over the ... See full document

25

Consistency and quality assessment of the Metop-A/IASI and Metop-B/IASI  operational trace gas products (O&lt;sub&gt;3&lt;/sub&gt;,  CO,  N&lt;sub&gt;2&lt;/sub&gt;O,   CH&lt;sub&gt;4&lt;/sub&gt;, and  CO&lt;sub&gt;2&lt;/sub&gt;) in the subtropical North Atlantic

Consistency and quality assessment of the Metop-A/IASI and Metop-B/IASI operational trace gas products (O<sub>3</sub>, CO, N<sub>2</sub>O, CH<sub>4</sub>, and CO<sub>2</sub>) in the subtropical North Atlantic

... consistent, and high-quality long-term monitor- ing of the composition of the atmosphere is fundamental for addressing the challenges of climate ...research. In this con- text ... See full document

19

Ability of the 4-D-Var analysis of the GOSAT BESD XCO&lt;sub&gt;2&lt;/sub&gt;  retrievals to characterize  atmospheric CO&lt;sub&gt;2&lt;/sub&gt; at large and  synoptic scales

Ability of the 4-D-Var analysis of the GOSAT BESD XCO<sub>2</sub> retrievals to characterize atmospheric CO<sub>2</sub> at large and synoptic scales

... Wunch, D., Wennberg, P. O., Toon, G. C., Connor, B. J., Fisher, B., Osterman, G. B., Frankenberg, C., Mandrake, L., O’Dell, C., Ahonen, P., Biraud, S. C., Castano, R., Cressie, N., Crisp, D., Deutscher, N. M., Eldering, ... See full document

19

The potential for regional-scale bias in top-down CO&lt;sub&gt;2&lt;/sub&gt; flux estimates due to atmospheric transport errors

The potential for regional-scale bias in top-down CO<sub>2</sub> flux estimates due to atmospheric transport errors

... J., and Denning, A. S.: Weak northern and strong tropical land carbon uptake from vertical profiles of atmospheric CO 2 , Science, 316, ... See full document

29

Global atmospheric carbon budget: results from an ensemble of atmospheric CO&lt;sub&gt;2&lt;/sub&gt; inversions

Global atmospheric carbon budget: results from an ensemble of atmospheric CO<sub>2</sub> inversions

... of the par- ticipating submissions varies considerably from the original 22 Transcom-3 land and ocean regions (JMA, TrC) to the transport model grid cells (LSCEa, MACC-II, JENA) (Ta- ... See full document

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