The general circulation model (GCM) of the Meteorological Office (NO), U.K., was used to investigate the impact of waste heat on simulated global climate. These experiments are a further set in a series of experiments made to investigate the behavior of the simulated circulation with different scenarios and energy releases. In contrast to the previous experiments, the heat is distributed only over continental areas, where large energy and/or population densities can be expected in the future. The results suggest that the atmosphere responds very sensitively to the distribution of the heat input. Although the total hemispheric changes are smaller than in some of the previous experiments, there are still considerable areas where the diffe...
We simulated anthropogenic global change through the entire atmosphere, including the thermosphere a...
This book seeks to assemble the scattered knowledge available to date on the interactions between tw...
Climate models based on global radiative equilibrium are normally so complicated that they require e...
Experiments were made with the Meteorological Office general circulation model (GCM) to investigate ...
The general circulation model (GCM) of the Meteorological Office, UK (UKMO), has been used to invest...
The general circulation model of the United Kingdom Meteorological Office (UKMO) has been used to in...
The general circulation model (GCM) of the United Kingdom Meteorological Office (UKMO) has been used...
There are three energy options which could satisfy a projected energy requirement of about 30 TW and...
Mathematical simulation of regional climate perturbation due to waste heat rejection using a hydrody...
Waste heat is a major source of recoverable loss in societal energy use, offering significant potent...
Cooling and darkening at Earth's surface are expected to result from the interception of sunlight by...
The energy sector is not only a major contributor to greenhouse gases, it is also vulnerable to clim...
Abstract. Heat waves and dry spells are analyzed (i) at eight stations in south Moravia (Czech Repub...
The IIASA Energy Program is studying global aspects of energy systems in terms of resources, demands...
An overview of boundary layer modelling is presented, which focusses on the description of the model...
We simulated anthropogenic global change through the entire atmosphere, including the thermosphere a...
This book seeks to assemble the scattered knowledge available to date on the interactions between tw...
Climate models based on global radiative equilibrium are normally so complicated that they require e...
Experiments were made with the Meteorological Office general circulation model (GCM) to investigate ...
The general circulation model (GCM) of the Meteorological Office, UK (UKMO), has been used to invest...
The general circulation model of the United Kingdom Meteorological Office (UKMO) has been used to in...
The general circulation model (GCM) of the United Kingdom Meteorological Office (UKMO) has been used...
There are three energy options which could satisfy a projected energy requirement of about 30 TW and...
Mathematical simulation of regional climate perturbation due to waste heat rejection using a hydrody...
Waste heat is a major source of recoverable loss in societal energy use, offering significant potent...
Cooling and darkening at Earth's surface are expected to result from the interception of sunlight by...
The energy sector is not only a major contributor to greenhouse gases, it is also vulnerable to clim...
Abstract. Heat waves and dry spells are analyzed (i) at eight stations in south Moravia (Czech Repub...
The IIASA Energy Program is studying global aspects of energy systems in terms of resources, demands...
An overview of boundary layer modelling is presented, which focusses on the description of the model...
We simulated anthropogenic global change through the entire atmosphere, including the thermosphere a...
This book seeks to assemble the scattered knowledge available to date on the interactions between tw...
Climate models based on global radiative equilibrium are normally so complicated that they require e...