Results 11 to 20 of about 5,307,850 (295)

Radiative forcing in the 21st century due to ozone changes in the troposphere and the lower stratosphere [PDF]

open access: yes, 2003
Radiative forcing due to changes in ozone is expected for the 21st century. An assessment on changes in the tropospheric oxidative state through a model intercomparison ("OxComp'') was conducted for the IPCC Third Assessment Report (IPCC-TAR).
Isaksen, I S A   +92 more
core   +5 more sources

Radiative forcing since preindustrial times due to ozone change in the troposphere and the lower stratosphere [PDF]

open access: yes, 2006
Changes in atmospheric ozone have occurred since the preindustrial era as a result of increasing anthropogenic emissions. Within ACCENT, a European Network of Excellence, ozone changes between 1850 and 2000 are assessed for the troposphere and the lower ...
Isaksen, I S A   +22 more
core   +7 more sources

Electromagnetic Cascade Emission from Neutrino-coincident Tidal Disruption Events

open access: yesThe Astrophysical Journal, 2023
The potential association between Tidal Disruption Events and high-energy astrophysical neutrinos implies the acceleration of cosmic rays. These accelerated particles will initiate electromagnetic (EM) cascades spanning from keV to GeV energies via the ...
Chengchao Yuan, Walter Winter
doaj   +1 more source

The I3RC - Bringing Together the Most Advanced Radiative Transfer Tools for Cloudy Atmospheres [PDF]

open access: yes, 2005
The interaction of clouds with solar and terrestrial radiation is one of the most important topics of climate research. In recent years it has been recognized that only a full three-dimensional (3D) treatment of this interaction can provide answers to ...
K. Franklin Evans   +113 more
core   +1 more source

Observational estimates of radiative forcing due to land use change in southwest Australia [PDF]

open access: yes, 2007
Radiative forcing associated with land use change is largely derived from global circulation models (GCM), and the accuracy of these estimates depends on the robustness of the vegetation characterization used in the GCMs.
Christopher, S.A.   +13 more
core   +1 more source

CFD prediction of coupled radiation heat transfer and soot production in turbulent flames [PDF]

open access: yes, 1996
The mechanisms governing the formation and destruction of soot in turbulent combustion are intimately coupled to thermal radiation due to the strong dependence of sooting processes and radiative loss on temperature.
Bressloff, N. W.
core   +7 more sources

CLEAR-SKY RADIATIVE AND TEMPERATURE EFFECTS OF DIFFERENT AEROSOL CLIMATOLOGIES IN THE COSMO MODEL

open access: yesGeography, Environment, Sustainability, 2018
We estimated the effects of the different aerosol climatologies in the COSMO mesoscale atmospheric model using long-term aerosol measurements and the accurate global solar irradiance observations at ground at the Moscow State University Meteorological ...
Natalia Chubarova   +5 more
doaj   +1 more source

Design of a radiative heat recuperator for steel processes [PDF]

open access: yesMATEC Web of Conferences, 2020
In recent years, there has been an increasing interest in the recovery of the waste heat of steel and glass processes. This work proposes a numerical study of a waste heat exchanger system for steel production processes.
Fernandez Arroiabe Peru   +7 more
doaj   +1 more source

Observations of diurnal and spatial variability of radiative forcing by equatorial deep convective clouds [PDF]

open access: yes, 2004
From geostationary satellite observations of equatorial Africa and the equatorial east Atlantic during May and June 2000 we explore the radiative forcing by deep convective cloud systems in these regions. Deep convective clouds (DCCs) are associated with
Nowicki, S.   +4 more
core   +1 more source

Indirect long-term global radiative cooling from NOx emissions [PDF]

open access: yes, 2001
Anthropogenic emissions of short‐lived, chemically reactive gases, such as NO x and CO, are known to influence climate by altering the chemistry of the global troposphere and thereby the abundance of the greenhouse gases O3, CH4 and the HFCs.
Wild, Oliver   +2 more
core   +5 more sources

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