Radiative forcing within the Last Interglacial
Sensitivity of Red Sea circulation to sea level and insolation forcing during the last interglacial
... Abstract. This study investigates the response of Red Sea circulation to sea level and insolation changes during termi- nation II and across the last interglacial, in comparison with termination I and the ...
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Lack of evidence for a substantial sea-level fluctuation within the Last Interglacial
... However, this requires a +2 to +3 o C Southern Ocean temperature anomaly, which is greater than the +1.2 o C recorded by the palaeo data 62 , but perhaps not implausible given the average 2.6 o C 2-sigma uncertainty ...
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A probabilistic assessment of sea level variations within the last interglacial stage
... The cryosphere is a complex system with inherent stochasticity, and it is unclear to what extent identical climatic forcings would gen- erate identical ice sheet responses. While the ∼ 130 m GSL change between glacial ...
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ANGEO - Radiative forcing by contrails
... measuring IWC inside a contrail, which are due to the shortcomings of the various sensors and the represent- ativity of such measurements in a contrail cloud which is highly heterogeneous spatially. Figure 2a shows the ...
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Total aerosol effect: radiative forcing or radiative flux perturbation?
... Fig. 1. Model, satellite and inverse estimates of the aerosol indirect effects over the last two decades. Per method or effects considered, each symbol represents one published estimate (one paper one vote). Blue ...
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Estimating the Effective Radiative Forcing of Contrail Cirrus
... within this work. The contrail cirrus simulations, yielded with differently scaled AEDT 2050 air traffic, are marked as ATR followed by the scaling factor. In total, seven RF adj simulations and four ERF ...
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Precipitation, radiative forcing and global temperature change
... ] Radiative forcing is a useful tool for predicting equilibrium global temperature ...and radiative transfer calculations are used to quantify and assess this dependency across a range of climate ...
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Two layers cloud radiative forcing model
... cloud radiative forcing ...radiative forcing. The experimental results are satisfied with the radiative transfer model when the cloud optical depth is within the range of 10 2 ...
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The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing
... timated by Bamber et al. (2013) (Fig. 13). The choice of this particular κ value is based on the discussion above (Sect. 3.4) for the LGM and is supported by the good agreement be- tween the simulated present-day ice ...
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The sensitivity of the Greenland Ice Sheet to glacial-interglacial oceanic forcing
... the last decades the Greenland Ice Sheet (GrIS) has experienced a gradually accelerating mass loss, in part due to the observed speed- up of several of Greenland’s marine-terminating ...in interglacial ...
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Influence of radiative forcing factors on ground–air temperature coupling during the last millennium: implications for borehole climatology
... OZ/AER forcing on the air and soil temperature responses over this region during indus- trial ...trend within the indus- trial period is only seen in the ALL-F and the OZ/AER-only ...
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Bounding global aerosol radiative forcing of climate change
... aerosol radiative forcing, but uncertainties remain ...aerosol radiative forcing over the industrial era based on multiple, traceable, and arguable lines of evidence, including modeling ...
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Determination of aerosol characteristics and direct radiative forcing at Pune
... Pawar et al., Aerosol and Air Quality Research, 12: 1166–1180, 2012 1170 Fig. 3. Diurnal variability of AOD at different wavelengths during winter and pre-monsoon seasons at NWC. columnar aerosol content, three height ...
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How warm was Greenland during the last interglacial period?
... (0.256 ‰) is only 0.5 ◦ C lower than the estimated LIG op- timum temperature and hence very comparable to the esti- mated LIG optimum temperature. In summary, the NGRIP LIG vs. preindustrial temperature increase ( + 5.2 ...
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Factors controlling the last interglacial climate as simulated by LOVECLIM1.3
... Clearly other sources of uncertainty, not studied here, such as uncertainties related to choices made in the representation of the model components, to their physical parameterisations and to the model resolution (Murphy ...
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Last interglacial temperature evolution – a model inter-comparison
... 2.3 Data processing All the simulated temperature fields were averaged into 50 yr averages for every month. For the CCSM3 and KCM simu- lations, which are performed with a 10-fold acceleration of the changes in the ...
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Last Interglacial sea-level proxies in the Western Mediterranean
... insights into the magnitude and the sea-level fluctuations within the MIS 5e in the western Mediterranean. A particular situation characterizes the coastal plains of the northwestern Adriatic Sea where, because of ...
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Importance of tropospheric volcanic aerosol for indirect radiative forcing of climate
... Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy ...
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Absorbing aerosols: contribution of biomass burning and implications for radiative forcing
... τ = β C · λ (−α C ) + β F · λ (−α F ) + τ BC (7) where subscript C denotes the coarse mode and F denotes fine mode. τ BC is the optical depth due to black carbon par- ticles. We use surface measurements of BC ...
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Wintertime aerosol optical properties and radiative forcing over rohtak
... Measurement site, Instrument and Methodology The experimental site Rohtak is located in the North-Western part of India (Lat 28.89°N, Long 76.58°E, 214m AMSL) 70 km northwest of Delhi. Like most Indian cities, Rohtak has ...
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