Sentence examples for mean temperature change from inspiring English sources

Different climate impact metrics were used (global mean temperature change, global warming potential and cumulative radiative forcing) and evaluations were made for single harvest as well as continuous supply over a landscape.

Therefore, its recorded summer temperature would play an immense importance for policy makers and other stakeholders in adapting and overcoming the consequences of the mean temperature change over the country.

Future monthly temperature variation about the ensemble mean temperature change is produced using normal random number generation, resulting in a possible future scenario of SST change with seasonal fluctuations constrained by the historical distributions (example, Fig. 5).

For instance, when these latitudinal regions were analyzed with respect to the percentage of area having experienced significant change, we found that the southern temperate region experienced the greatest area of significant mean temperature change (62%).

All AOGCM bias-corrected SST predictions at each location that passed selection criteria (the same as that defined above) were low-pass filtered to remove the model-imposed seasonal fluctuations and then averaged, resulting in a multi-model mean temperature change (increase) for years 2000 2099 for each location.

When the temperature was out of range, the mean temperature change from target was calculated.

Fig. 2 Global and annual mean temperature changes from the preindustrial control simulation in the MIROC3.2 (medres) AOGCM experiments.

As an example, we focus on the response to solar and volcanic forcing in the context of the Maunder Minimum, a cool period of the late 17th century and demonstrate that although (northern) hemispheric mean temperature changes can be reasonably simulated in most models, the details of regional patterns depend more heavily on the included physics.

By plotting climate change as a function of the mean latitude of each country, we demonstrate that countries located in northern latitudes tended to have a greater proportion of their area (i.e., grid cells) experiencing significant annual mean temperature changes greater than 0.4°C/decade (Figure 4, top).

During the Development Phase, from Onset to Peak, humidity steeply rises, whereas mean temperature changes minimally in a slow decline.

The projected annual mean temperature changes in the A1B scenario, with respect to the period 1961 1990 are shown in Figure 1.