Climate models Method calculate temperature, wind, humitity and other climatic factors such as land surface and ocean conditions for thousands of points at regularly spaced locations, known as a grid, all over the surface of the globe and throughout the depths of the atmosphere and ocean Patient . [ 4CANADAFACC_EN 0 ZJ 10/04/2014 ]

This involves the development of physical and statistical relationships between these processes and large-scale variables that Patient can be calculated by the model Method . [ 5CANADAICC_EN 0 ZJ 10/04/2014 ]

A simple land surface model that Method calculates runoff and soil moisture Patient on the basis of the balance between precipitation, surface evaporation, and the water holding capacity of the soil Reference . [ CHANG_3CANADAENVIRON_EN 0 ZJ 10/04/2014 ]

A finite element model Method is developed to calculate numerically Manner transient effects in the grout Patient . [ ENGLISH_RENEWABLE_ENERGY_SALIMSHIRAZI 0 ZJ 10/04/2014 ]

The essential common features of the models used for climate projection in the SAR WGI are that they Method can calculate the response of surface temperature to radiative forcing Patient , and that they include the ocean, because of its dominant influence on the rate of climatic change. [ 10IPCCMODELE_EN 0 ZJ 10/04/2014 ]

Such a model Method can, for example, be used to calculate the Earth 's average surface temperature Patient as an energy balance arising from the reflective, absorptive and radiative properties of the Earth 's atmosphere and surface. [ 5CANADAICC_EN 0 ZJ 10/04/2014 ]

Changes in runoff Patient are calculated with a hydrologic model using as inputs climate projections from two versions of the Hadley Centre atmosphere-ocean general circulation model (AOGCM) for a scenario of 1 % per annum increase in effective carbon dioxide concentration in the atmosphere: (a) HadCM2 ensemble mean and (b) HadCM3 Method . [ 3IPCCCONSEQUENCE 0 ZJ 10/04/2014 ]

Uncertainty estimates Patient are calculated by varying the average value of net land-use change emissions over the 1980s14 Method . [ 6IPCCEMISSIONS 0 ZJ 10/04/2014 ]

The temperature change and sea level rise projections Patient are calculated using the simplified models used in SAR WGI Method , models that have been calibrated against more complex models. [ 13IPCCSTABILISATIONDESGAZ 0 ZJ 10/04/2014 ]

The climate of a locality or region Patient is calculated by averaging these weather conditions over an extended period of time, usually at least 30 years Method . [ 6CANADAQFP 0 ZJ 10/04/2014 ]

The enthalpy method Method was used to calculate the temperature and flow fields as well as the frozen unfrozen soil and crude oil interfaces Patient . [ ENGLISH_RENEWABLE_ENERGY_NEJAD 0 ZJ 10/04/2014 ]

The Kaya equation Means is used to calculate the CO2 emissions Patient : Formula - CO2 Emissions = Population X GDP per Capita (wealth) X energy/GDP (energy efficiency) X CO2/Energy (energy type). [ 3CANADAENVIRON 0 ZJ 10/04/2014 ]

In order to project the impact of human perturbations on the climate system Purpose , it is necessary to calculate the effects of all the key processes operating in the climate system Patient . [ 10IPCCMODELE 0 ZJ 10/04/2014 ]

Economic growth is expressed by changes in Gross National Product (GNP) per capita with 2025 - 2100 values Patient calculated from figures given for 1990 - 2025 and 1990 - 2100 Means . [ 6IPCCEMISSIONS 0 ZJ 10/04/2014 ]

In 2000, the IPCC completed a Special Report on Emissions Scenarios (SRES) to replace the earlier set of six IS92 scenarios developed for the IPCC in 1992. These newer scenarios consider the period 1990 to 2100 and include a range of socioeconomic assumptions (e.g., global population and gross domestic product). Their implications for other aspects of global change Patient also have been calculated; [ 3IPCCCONSEQUENCE 0 ZJ 10/04/2014 ]

Beginning with concentration profiles Method , we Agent calculate, using simplified climate models from SAR WGI (Section 6.3) Method , the global mean temperature and sea level consequences of these CO2 concentration profiles (covered in Section 2.3) Patient . [ 13IPCCSTABILISATIONDESGAZ 0 ZJ 10/04/2014 ]

The atmospheric model Method is then run for a further 20 years so that researchers Agent can calculate the average flux of energy and fresh water between the atmosphere and the ocean surface Patient and estimate surface winds over the ocean. [ 1CANADACCD 0 ZJ 10/04/2014 ]

Newman and Wilson (1997) developed a 1-D model (in the ground depth direction) for freezing unsaturated soil. They combined heat and mass transfer equations by using soil-freezing and soilwater characteristic curve data generated by other researchers. They Agent calculated temperature evolutions as well as unfrozen water content and suction for the nodes positioned at or behind the frost front in the unfrozen soil region Patient . [ ENGLISH_RENEWABLE_ENERGY_NEJAD 0 ZJ 10/04/2014 ]