Earth's energy balance since 1950
Tags: ENERGY budget (Geophysics); EARTH temperature; CLIMATOLOGY; RADIATIVE forcing; AEROSOLS (Sprays) -- Environmental aspects; CLIMATIC changes -- Detection
Related Articles
- Incoming Solar and Infrared Radiation Derived from METEOSAT: Impact on the Modeled Land Water and Energy Budget over France. Carrer, D.; Lafont, S.; Roujean, J.-L.; Calvet, J.-C.; Meurey, C.; Le Moigne, P.; Trigo, I. F. // Journal of Hydrometeorology;Apr2012, Vol. 13 Issue 2, p504
The Land Surface Analysis Satellite Applications Facility (LSA SAF) project radiation fluxes, derived from the Meteosat Second Generation (MSG) geostationary satellite, were used in the Interactions between Soil, Biosphere, and Atmosphere (ISBA) land surface model (LSM), which is a component of...
- A transitioning Arctic surface energy budget: the impacts of solar zenith angle, surface albedo and cloud radiative forcing. Sedlar, Joseph; Tjernstr�m, Michael; Mauritsen, Thorsten; Shupe, Matthew; Brooks, Ian; Persson, P.; Birch, Cathryn; Leck, Caroline; Sirevaag, Anders; Nicolaus, Marcel // Climate Dynamics;Oct2011, Vol. 37 Issue 7/8, p1643
Snow surface and sea-ice energy budgets were measured near 87.5�N during the Arctic Summer Cloud Ocean Study (ASCOS), from August to early September 2008. Surface temperature indicated four distinct temperature regimes, characterized by varying cloud, thermodynamic and solar properties. An...
- Technical Note: a combined SBUV and SAGE zonal-mean ozone data set. McLinden, C. A.; Tegtmeier, S.; Fioletov, V. // Atmospheric Chemistry & Physics Discussions;2009, Vol. 9 Issue 3, p12385
A stratospheric monthly, zonal-mean combined ozone data set based on Satellite Aerosol and Gas Experiment (SAGE) and Solar Backscatter UltraViolet (SBUV) data spanning 1978-2005 is presented. Drifts in individual SBUV instruments and inter-SBUV biases are corrected using SAGE I and II by...
- Testing for the Possible Influence of Unknown Climate Forcings upon Global Temperature Increases from 1950 to 2000. Anderson, Bruce T.; Knight, Jeff R.; Ringer, Mark A.; Yoon, Jin-Ho; Cherchi, Annalisa // Journal of Climate;Oct2012, Vol. 25 Issue 20, p7163
Global-scale variations in the climate system over the last half of the twentieth century, including long-term increases in global-mean near-surface temperatures, are consistent with concurrent human-induced emissions of radiatively active gases and aerosols. However, such consistency does not...
- Direct Aerosol Radiative Forcing Uncertainty Based on a Radiative Perturbation Analysis. Loeb, Norman G.; Wenying Su // Journal of Climate;Oct2010, Vol. 23 Issue 19, p5288
To provide a lower bound for the uncertainty in measurement-based clear- and all-sky direct aerosol radiative forcing (DARF), a radiative perturbation analysis is performed for the ideal case in which the perturbations in global mean aerosol properties are given by published values of systematic...
- An Indirect Effect of Ice Nuclei on Atmospheric Radiation. Zeng, Xiping; Tao, Wei-Kuo; Zhang, Minghua; Hou, Arthur Y.; Xie, Shaocheng; Lang, Stephen; Li, Xiaowen; Starr, David O'C.; Li, Xiaofan; Simpson, Joanne // Journal of the Atmospheric Sciences;Jan2009, Vol. 66 Issue 1, p41
A three-dimensional cloud-resolving model (CRM) with observed large-scale forcing is used to study how ice nuclei (IN) affect the net radiative flux at the top of the atmosphere (TOA). In all the numerical experiments carried out, the cloud ice content in the upper troposphere increases with IN...
- Quantification of DMS aerosol-cloud-climate interactions using ECHAM5-HAMMOZ model in current climate scenario. Thomas, M. A.; Suntharalingam, P.; Pozzoli, L.; Rast, S.; Devasthale, A.; Kloster, S.; Feichter, J.; Lenton, T. M. // Atmospheric Chemistry & Physics Discussions;2010, Vol. 10 Issue 2, p3087
The contribution of ocean dimethyl sulfide (DMS) emissions to changes in cloud microphysical properties is quantified seasonally and globally for present day climate conditions using an aerosol-chemistry-climate general circulation model, ECHAM5-HAMMOZ, coupled to a cloud microphysics scheme. We...
- Detection of dust aerosol by combining CALIPSO active lidar and passive IIR measurements. Chen, B.; Huang, J.; Minnis, P.; Hu, Y.; Yi, Y.; Liu, Z.; Zhang, D.; Wang, X. // Atmospheric Chemistry & Physics Discussions;2010, Vol. 10 Issue 2, p3423
The version 2 Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) dust layer detection method, which is based only on lidar measurements, misclassified about 43% dust layers (mainly dense dust layer) as cloud layers over the Taklamakan Desert. To address this problem, a...
- Bromine measurements in ozone depleted air over the Arctic Ocean. Neuman, J. A.; Nowak, J. B.; Huey, L. G.; Burkholder, J. B.; J. E.6Dibb; Holloway, J. S.; Liao, J.; Peischl, J.; Roberts, J. M.; Ryerson, T. B.; Scheuer, E.; Stark, H.; Stickel, R. E.; Tanner, D. J.; Weinheimer, A. // Atmospheric Chemistry & Physics Discussions;2010, Vol. 10 Issue 2, p3827
In situ measurements of ozone, photochemically active bromine compounds, and other trace gases over the Arctic Ocean in April 2008 are used to examine the chemistry and geographical extent of ozone depletion in the arctic marine boundary layer (MBL). Data were obtained from the NOAA WP-3D...
