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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 359 (1992), S. 117-122 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Global cooling in the Cenozoic, which led to the growth of large continental ice sheets in both hemispheres, may have been caused by the uplift of the Tibetan plateau and the positive feedbacks initiated by this event. In particular, tectonically driven increases in chemical weathering may have ...
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 3 (1980), S. 65-87 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Six northeast Atlantic cores contain planktonic foraminiferal records implying a very abrupt glacial/interglacial surface-ocean warming roughly coincident with the last deglaciation (isotopic termination II) at 127 000 yr B.P. These faunal composition curves have, however, been substantially altered by sediment mixing processes on the sea floor; they are translated downward in the core record and made to look steeper than they actually were. The reason for this abnormally large mixing impact is an interval of sediment with very low to negligible concentrations of all microfossils (surface ocean and bottom living). These low concentrations reflect a several-thousand-year interval of low productivity and little or no life in the overlying surface waters. We interpret this thorough suppression of productivity as a consequence of meltwater and icebergs flooding into the subpolar Atlantic gyre from the surrounding Northern Hemisphere ice sheets during deglaciation. The meltwater influx inhibited warm-season productivity by maintaining a well-stratified low-salinity surface layer; in winter, the low salinity layer froze, stopping nutrientrich deep waters from surfacing in normal cold-season convection. The earth's orbital configuration during this deglaciation created an unusually strong summer insolation maximum and winter insolation minimum in the Northern Hemisphere. Rapid melting and disintegration of the Northern Hemisphere ice sheets induced by strong summer insolation apparently created the meltwater influx; combined with very low winter insolation, the presence of this low-salinity meltwater layer led to unusually extensive sea-ice formation. The existence of a large region of winter sea ice across the subpolar North Atlantic during deglaciation implies a reduced supply of moisture in winter to the wasting Northern Hemisphere ice sheets. This includes the loss of winter moisture both locally from ice-covered northern waters and regionally from low-latitude winter storms no longer penetrating northward. The winter sea-ice cover thus acts as an amplifier providing positive feedback to the insolation-driven deglaciation process.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 3 (1990), S. 65-87 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Six northeast Atlantic cores contain planktonic foraminiferal records implying a very abrupt glacial/interglacial surface-ocean warming roughly coincident with the last deglaciation (isotopic termination II) at 127 000 yr B.P. These faunal composition curves have, however, been substantially altered by sediment mixing processes on the sea floor; they are translated downward in the core record and made to look steeper than they actually were. The reason for this abnormally large mixing impact is an interval of sediment with very low to negligible concentrations of all microfossils (surface ocean and bottom living). These low concentrations reflect a several-thousand-year interval of low productivity and little or no life in the overlying surface waters. We interpret this thorough suppression of productivity as a consequence of meltwater and icebergs flooding into the subpolar Atlantic gyre from the surrounding Northern Hemisphere ice sheets during deglaciation. The meltwater influx inhibited warm-season productivity by maintaining a well-stratified low-salinity surface layer; in winter, the low salinity layer froze, stopping nutrientrich deep waters from surfacing in normal cold-season convection. The earth's orbital configuration during this deglaciation created an unusually strong summer insolation maximum and winter insolation minimum in the Northern Hemisphere. Rapid melting and disintegration of the Northern Hemisphere ice sheets induced by strong summer insolation apparently created the meltwater influx; combined with very low winter insolation, the presence of this low-salinity meltwater layer led to unusually extensive sea-ice formation. The existence of a large region of winter sea ice across the subpolar North Atlantic during deglaciation implies a reduced supply of moisture in winter to the wasting Northern Hemisphere ice sheets. This includes the loss of winter moisture both locally from ice-covered northern waters and regionally from low-latitude winter storms no longer penetrating northward. The winter sea-ice cover thus acts as an amplifier providing positive feedback to the insolation-driven deglaciation process.
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  • 4
    Publication Date: 2011-07-30
    Description: Neotropical biomass burning reconstructions synthesized from soil and sedimentary charcoal records indicate a period of reduced biomass burning sustained for several centuries after ~500 cal. yr BP. Proxy records of solar irradiance, El Niño events, temperature, and precipitation document regionally variable climate-related trends that do not account for the uniform reduction in burning across the Neotropics. Decreased human ignition resulting from pandemic-induced mortality offers an alternative, geographically comprehensive explanation. In addition, natural (solar-volcanic) factors can explain only ~1.3 ppm out of the rapid 6–10 ppm CO 2 decrease between ad 1525 and the early 1600s. Reforestation following land abandonment due to population collapse has the potential to account for the rest of this CO 2 decline, and variations in the 13 C/ 12 C of atmospheric CO 2 and CH 4 are consistent with both a major reduction in Neotropical landscape management by fire and massive reforestation. Our findings are demonstrative of the scale at which pre-industrial human activities influenced Earth’s atmospheric greenhouse gas budget.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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  • 5
    Publication Date: 2011-07-30
    Description: We compare climate simulations for Present-Day (PD), Pre-Industrial (PI) time, and a hypothetical (inferred) state termed No-Anthropogenic (NA) based upon the low greenhouse gas (GHG) levels of the late stages of previous interglacials that are comparable in time (orbital configuration) to the present interglacial. We use a fully coupled dynamical atmosphere–ocean model, the CCSM3. We find a consistent trend toward colder climate (lower surface temperature, more snow and sea-ice cover, lower ocean temperature, and modified ocean circulation) as the net change in GHG radiative forcing trends more negative from PD to PI to NA. The climatic response of these variables becomes larger relative to the changed GHG forcing for each step toward a colder climate state (PD to PI to NA). This amplification is significantly enhanced using the dynamical atmosphere–ocean model compared with our previous results with an atmosphere–slab ocean model, a result that conforms to earlier idealized GHG forcing experiments. However, in our case this amplification is not an idealized result, but instead helps frame important questions concerning aspects of Holocene climate change. This enhanced amplification effect leads to an increase in our estimate of the climate’s response to inferred early anthropogenic CO 2 increases (NA to PI) relative to the response to industrial-era CO 2 increases (PI to PD). Although observations of the climate for the hypothetical NA (inferred from observations of previous interglacials) and for PI have significant uncertainties, our new results using CCSM3 are in better agreement with these observations than our previous results from an atmospheric model coupled to a static slab ocean. The results support more strongly inferences by Ruddiman concerning indirect effects of ocean solubility/sea-ice/deep ocean ventilation feedbacks that may have contributed to a further increase in late-Holocene atmospheric CO 2 beyond that caused by early anthropogenic emissions alone.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
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  • 6
    Publication Date: 2011-07-30
    Description: We test the influence of model resolution on glacial inception using a coupled atmosphere–slab ocean version of NCAR’s CCSM3 GCM. Simulations employ a modern orbital configuration and greenhouse gas concentrations representing both recent (year 1990) and hypothetically lower values based on Ruddiman’s Early Anthropogenic Hypothesis (240 ppm CO 2 , 450 ppb CH 4 ). We ran the model at two different horizontal resolutions: relatively coarse (spectral T42, approximately 2.8°) and comparatively fine (T85, approximately 1.4°). Under contemporary greenhouse forcing, permanent boreal snow cover extent in the two model configurations is similar, but lowering greenhouse gas concentrations generates much more extensive glacial inception in the T85 experiment (150% increase) than at T42 resolution (80% increase). Furthermore, the spatial patterns of glacial inception differ considerably. Only the T85 version produces permanent snow cover over the Rocky Mountains and Baffin Island, consistent with geologic evidence for early glaciation in the northern Rockies and Laurentide ice sheet nucleation in northeastern Canada. Although enhanced sensitivity at higher resolution is largely attributable to the expected colder and wetter conditions over elevated topography, much of the response is also driven dynamically. Atmospheric pressure changes at the surface and aloft differ considerably between model resolutions. The T85 circulation anomalies favor a stronger onshore moisture flux and therefore more snowfall over the northern Rockies and Baffin Island. Although these experiments are driven by greenhouse forcing rather than orbital anomalies, our findings may apply to general mechanisms of glacial inception.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
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  • 7
    Publication Date: 2011-07-30
    Description: Concentrations of CO 2 and CH 4 in the atmosphere rose slowly during the millennia prior to the industrial era. Opposing explanations for these increases have invoked natural and anthropogenic sources. Here we revisit this argument using new evidence to see whether either explanation can be falsified (disproven, in the sense proposed by German philosopher Karl Popper). Two lines of evidence suggest that natural explanations for the CH 4 increase are falsified: (1) the absence of any sustained methane increase early in seven interglaciations prior to the Holocene; and (2) weakening emissions during the last 5000 years from the two largest global sources of CH 4 – north tropical and boreal wetlands. Consistent with this interpretation, a new synthesis of archeological data from southern Asia reported in this issue indicates an exponential increase in CH 4 emissions from expanding rice irrigation during the last 5000 years. Neither the anthropogenic nor the natural explanations for the CO 2 increase can at this point be falsified. Previous studies that rejected the early anthropogenic hypothesis based on the small size of early farming populations ignored a rich array of archeological and historical evidence showing that early farmers used much more land per capita than those in the centuries just before the industrial era. Previous interpretations of very small terrestrial (anthropogenic and other) carbon emissions during the last 7000 years based on the 13 CO 2 record failed to incorporate credible estimates of very large carbon burial in boreal peat lands during the late Holocene. Allowance for larger burial in peat deposits requires much greater emissions of anthropogenic carbon to balance the 13 CO 2 budget. The prevalence of downward CO 2 trends during equivalent intervals early in previous interglaciations poses a major problem for natural explanations of the late-Holocene CO 2 increase.
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    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
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  • 8
    Publication Date: 2011-07-30
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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  • 9
    Publication Date: 2011-07-30
    Description: Humans have altered the Earth’s land surface since the Paleolithic mainly by clearing woody vegetation first to improve hunting and gathering opportunities, and later to provide agricultural cropland. In the Holocene, agriculture was established on nearly all continents and led to widespread modification of terrestrial ecosystems. To quantify the role that humans played in the global carbon cycle over the Holocene, we developed a new, annually resolved inventory of anthropogenic land cover change from 8000 years ago to the beginning of large-scale industrialization ( ad 1850). This inventory is based on a simple relationship between population and land use observed in several European countries over preindustrial time. Using this data set, and an alternative scenario based on the HYDE 3.1 land use data base, we forced the LPJ dynamic global vegetation model in a series of continuous simulations to evaluate the impacts of humans on terrestrial carbon storage during the preindustrial Holocene. Our model setup allowed us to quantify the importance of land degradation caused by repeated episodes of land use followed by abandonment. By 3 ka BP, cumulative carbon emissions caused by anthropogenic land cover change in our new scenario ranged between 84 and 102 Pg, translating to c . 7 ppm of atmospheric CO 2 . By ad 1850, emissions were 325–357 Pg in the new scenario, in contrast to 137–189 Pg when driven by HYDE. Regional events that resulted in local emissions or uptake of carbon were often balanced by contrasting patterns in other parts of the world. While we cannot close the carbon budget in the current study, simulated cumulative anthropogenic emissions over the preindustrial Holocene are consistent with the ice core record of atmospheric 13 CO 2 and support the hypothesis that anthropogenic activities led to the stabilization of atmospheric CO 2 concentrations at a level that made the world substantially warmer than it otherwise would be.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
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  • 10
    Publication Date: 1992-09-01
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Springer Nature
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