Natural and anthropogenic changes in atmospheric CO2over the last 1000 years from air in Antarctic ice and firn - Wikidata - wikimedia - TriplyDB

Natural and anthropogenic changes in atmospheric CO2over the last 1000 years from air in Antarctic ice and firn

Natural and anthropogenic changes in atmospheric CO2over the last 1000 years from air in Antarctic ice and firn

http://www.wikidata.org/entity/Q55919755

about

Rapid atmospheric CO2 changes associated with the 8,200-years-B.P. cooling event.Geoengineering potential of artificially enhanced silicate weathering of olivine Contributions to accelerating atmospheric CO2 growth from economic activity, carbon intensity, and efficiency of natural sinks Global and regional drivers of accelerating CO2 emissions The Influences of Drought and Land-Cover Conversion on Inter-Annual Variation of NPP in the Three-North Shelterbelt Program Zone of China Based on MODIS Data A new positive relationship between pCO2 and stomatal frequency in Quercus guyavifolia (Fagaceae): a potential proxy for palaeo-CO2 levels Larger CO₂ source at the equatorial Pacific during the last deglaciation Megacycles of atmospheric carbon dioxide concentration correlate with fossil plant genome size Carbon dioxide and the uneasy interactions of trees and savannah grasses Rates of change in natural and anthropogenic radiative forcing over the past 20,000 years Trends of measured climate forcing agents Estimating climate change, CO2 and technology development effects on wheat yield in northeast Iran.Climate change in the Fertile Crescent and implications of the recent Syrian drought A climate-change risk analysis for world ecosystems.No growth stimulation of Canada's boreal forest under half-century of combined warming and CO2 fertilization A role for atmospheric CO2 in preindustrial climate forcing.Nitrogen assimilation and growth of wheat under elevated carbon dioxide.First synchronous retreat of ice shelves marks a new phase of polar deglaciation Sensitivity of plants to changing atmospheric CO2 concentration: from the geological past to the next century.Trade-Offs between Growth Rate, Tree Size and Lifespan of Mountain Pine (Pinus montana) in the Swiss National Park.Ecophysiology matters: linking inorganic carbon acquisition to ecological preference in four species of microalgae (Chlorophyceae).Changes in biomass allocation buffer low CO2 effects on tree growth during the last glaciation.Native American depopulation, reforestation, and fire regimes in the Southwest United States, 1492-1900 CE Surrogate gas prediction model as a proxy for Δ14C-based measurements of fossil fuel-CO2.Global emissions of terpenoid VOCs from terrestrial vegetation in the last millennium.Diversity in plant hydraulic traits explains seasonal and inter-annual variations of vegetation dynamics in seasonally dry tropical forests.Changes in C uptake in populations of Chlamydomonas reinhardtii selected at high CO2.Protective role of carbon dioxide (CO2) in generation of reactive oxygen species.Ring-opening polymerization reactions of propylene oxide catalyzed by porphyrin metal 3+ complexes of aluminum, chromium and cobalt.Glacial trees from the La Brea tar pits show physiological constraints of low CO₂.Pyrrolic-nitrogen doped graphene: a metal-free electrocatalyst with high efficiency and selectivity for the reduction of carbon dioxide to formic acid: a computational study.The carbon sink in intact tropical forests.Greenhouse gases in the Earth system: a palaeoclimate perspective.Modelling terrestrial nitrous oxide emissions and implications for climate feedback.Anthropogenic and solar forcing in δ13C time pattern of coralline sponges.Determining climate change impacts on ecosystems: the role of palaeontology Ocean circulation and biogeochemistry moderate interannual and decadal surface water pH changes in the Sargasso Sea Colonization of the Americas, ‘Little Ice Age’ climate, and bomb-produced carbon: Their role in defining the Anthropocene Positive feedback between global warming and atmospheric CO2concentration inferred from past climate change Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice

P2860

Q24535747-1ABCAAF9-670A-4011-B8D4-B93181DE544A Q24631462-23560FDE-D265-4671-8A6B-C34CD85CED92 Q24676455-02C744C0-3CB9-4B47-8E7B-46776F29616E Q24682003-01AAEFFC-4A46-44F5-B4C6-5AC3BDA82F83 Q28597223-D6C1A6E4-935E-4F1B-861F-330C843F25FE Q28651619-7E874097-10A1-4AEE-A89B-0402E0BC0430 Q28658467-F4D608A6-CC19-450B-877D-BCD067A85131 Q28740617-9BC52D98-9081-408C-8428-C133F1ED14EB Q28740629-9DE57712-7760-42FD-88E8-91BC606ADF39 Q28755714-B2B7132E-2C52-4E25-B871-97985E80CD9A Q28775665-DE3F80CA-F506-4B9F-A145-A11E992D0535 Q30587630-70F3BB5B-C85C-4F37-92D1-52B20D926C07 Q30903095-D3695A21-BF02-4394-8819-742E116C8C04 Q31056084-805BF493-EF0C-4DED-86BB-0CC3899C263E Q31148390-1A129500-227C-4458-A507-1AE67542D6C3 Q33374237-A359A939-AB8F-44DF-8680-626B6AC1E149 Q34010832-E3B0AA51-800B-49CA-8A6E-EE6B9C9E0F44 Q34074638-254C5B5D-DA3C-45CB-89E7-A9E01DC02135 Q34560915-8317E38D-7486-4DA5-82F6-4BBB42A972F1 Q35940964-8B733753-6489-44AA-98AE-18B6E3EC9F3F Q36131818-B891B9A1-08C8-4077-B440-C831815B94E9 Q36289242-590E9660-6940-4C04-BDDA-5907930BA6A8 Q36598803-163FF039-FE66-4455-BA9B-312ABDB57845 Q37626757-0F4C7081-2C4F-4DC2-BD19-2D995656CB4D Q38859423-B5048C6A-10B2-4E39-80B5-605C2FCF5940 Q39609059-E11C9FD5-F5EE-42A6-9281-BE376B80668B Q40297172-59ACB14C-CB29-414C-AAF1-5C2AD1F511CD Q40921006-5F6EFD1D-ECBB-412B-8FFF-53C9BB6F7E92 Q44786758-A9872848-0E23-431F-B346-4882F98BF490 Q46504634-E0152CC8-4781-4A6D-BAA4-65D0F9AB06D7 Q46598025-CA3EBD8A-20EF-4F71-BDCE-2F8B114A3011 Q46635323-4484E972-E2A8-4931-8726-248D2658C79E Q47253695-FE3D2A74-3A0A-48C6-BAC8-3B390BC76AAB Q48135885-F0019413-00ED-49AA-92D5-7EC71B6DB87C Q51430475-92466755-C945-41B3-ABA9-C9AA17330655 Q53100128-3AE3D88C-35F8-4502-A98C-F03A99EA6094 Q54996849-0017D318-578D-4125-934B-F869FD604B7E Q55628017-8B9EDEF4-9D0E-48BF-952E-16DB2697C9FF Q55877575-BD4DE3C7-C865-4683-B02C-37F59878C51C Q55921479-911BE773-BAC3-4626-A674-1BA479AF92B0

P2860

Natural and anthropogenic changes in atmospheric CO2over the last 1000 years from air in Antarctic ice and firn

http://www.wikidata.org/entity/Q55919755

description

im Februar 1996 veröffentlichter wissenschaftlicher Artikel

@de

wetenschappelijk artikel

@nl

наукова стаття, опублікована в лютому 1996

@uk

name

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@en

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@nl

type

label

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@en

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@nl

prefLabel

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@en

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@nl

P1433

Q55919755-AA9F9838-5121-4F98-A8E4-677F7188A28B

P1476

Q55919755-6182E3C7-AEA2-4859-AA9A-4C110047AA18

P2093

Q55919755-20C7B552-D5DC-4F4A-8E03-DEE1B64AA344

Q55919755-38E91B10-90C7-4C4A-AD1A-55B71400228A

Q55919755-810BADAD-FC5F-4038-9E89-DA24D793EFFE

Q55919755-8A2BCA03-DCA1-4886-9D3E-1172D1C6BF6D

Q55919755-933D20DF-AC4D-4313-BB73-7F8FB6EFCE8A

Q55919755-CA33B6C5-9D6C-45FB-905A-55747F09F3CA

P2860

Q55919755-050A9538-9EB1-4940-853A-47717EBF20C3

Q55919755-09D68026-F589-44B9-8D29-2C1D7AD68B63

Q55919755-23C51984-EFC4-4A1A-8F7C-B73BFC3156B4

Q55919755-331AD681-FC77-4F1A-808D-579639852C1C

Q55919755-4FAE03BA-CC01-4D0A-B545-74D109840D35

Q55919755-834A1B41-69E1-4851-AA94-050975C96021

Q55919755-988C88A5-0227-475E-854F-07CBF5C24FC9

Q55919755-A7933072-1340-43F5-A343-C861B1F80E33

Q55919755-A87216F9-F320-43F4-9B69-4CE506D35C3B

Q55919755-B9CA52D4-5821-416C-85DD-09647EB89416

P304

Q55919755-894C40E7-7427-45B8-A801-32BF546C42E4

P31

Q55919755-9A7A2011-0DFF-493A-90FF-9917BCB1531C

P356

Q55919755-1860A42F-666C-4DB4-BBDF-464019490917

P407

Q55919755-1DACA9B1-66A1-4997-A54F-74896FFD9514

P433

Q55919755-323D4544-2B90-4C06-A2FF-E838434F706D

P478

Q55919755-1B8D910A-452D-4C37-8346-007579000B4B

P577

Q55919755-18D85BE6-113A-445C-ADFB-0AD72001DF0A

P356

P1433

Journal of Geophysical Research

P1476

Natural and anthropogenic chan ...... air in Antarctic ice and firn

@en

P2093

D. M. Etheridge

http://www.w3.org/2001/XMLSchema#string

J.-M. Barnola

http://www.w3.org/2001/XMLSchema#string

L. P. Steele

http://www.w3.org/2001/XMLSchema#string

R. J. Francey

http://www.w3.org/2001/XMLSchema#string

R. L. Langenfelds

http://www.w3.org/2001/XMLSchema#string

V. I. Morgan

http://www.w3.org/2001/XMLSchema#string

P2860

Gravitational separation of gases and isotopes in polar ice caps.

Vostok ice core provides 160,000-year record of atmospheric CO2

Evidence from polar ice cores for the increase in atmospheric CO2 in the past two centuries

Climatic, edaphic, and biotic controls over storage and turnover of carbon in soils

Ice core sample measurements give atmospheric CO2 content during the past 40,000 yr

Ice core record of the 13C/12C ratio of atmospheric CO2 in the past two centuries

Evidence of changing concentrations of atmospheric CO2, N2O and CH4 from air bubbles in Antarctic ice

An Antarctic ice core reveals atmospheric CO2 variations over the past few centuries

CO2 record in the Byrd ice core 50,000–5,000 years bp

Age difference between polar ice and the air trapped in its bubbles

P304

4115-4128

http://www.w3.org/2001/XMLSchema#string

P31

scholarly article

P356

10.1029/95JD03410

http://www.w3.org/2001/XMLSchema#string

P407

P433

D2

http://www.w3.org/2001/XMLSchema#string

P478

101

http://www.w3.org/2001/XMLSchema#string

P577

1996-02-01T00:00:00Z

http://www.w3.org/2001/XMLSchema#dateTime