Sentence examples for distribution of insolation from inspiring English sources

The two principal mechanisms by which the orbital effects on the regional/seasonal distribution of insolation instigate climate change are melting/growth of ice sheets (thus albedo change –> temperature change) and the slow feedback effect of GHGs responding to temperature change, thus increasing the greenhouse effect.

Orbital parameters that vary over time, including eccentricity, obliquity and precession result in low-frequency variability in the seasonal-latitudinal distribution of insolation as shown in Fig. 1 (Kaufman et al. 2009; Schmidt et al. 2011).

It has been widely demonstrated that Earth's astronomical parameters (precession, obliquity, and eccentricity) control Earth's climate through changes in temporal and spatial distribution of insolation on the Earth's surface (e.g., Milankovitch, 1941; Hays et al., 1976; Berger et al., 1989).

A MATLAB™ program has been used to build the annual frequency distribution of hourly insolation over any module plane at a given location.

The robust seasonal asymmetry in the Asian monsoon response among the climate models is qualitatively reproduced by an AOGCM simulation forced by orbital parameters, suggesting that the seasonal-latitudinal distribution of the insolation anomaly is important to the centennial variability of the seasonal transition of the Asian monsoon.

For Building Integrated Photo Voltaic (BIPV) installation, similar statistical analysis has been carried out for the composite frequency distribution, which is formed by weighted summation of insolation distributions for different module planes used in the installation.

Descriptive statistics and scatter plot analysis revealed no evidence of non-normality in the distribution of asthma prevalence, geographical coordinates, insolation, air temperature, and air pollution data, allowing the use of linear regression analysis models to evaluate the relationships between the studied variables.

The distribution of solar radiation is known as the insolation pattern, and it is strongly affected by the geometry of Earth's orbit around the Sun and by the orientation, or tilt, of Earth's axis relative to the direct rays of the Sun.

Our results show that, even though the changes in the land sea contrast that drive the monsoon flow follow quite well the differences in the insolation forcing, the regional distribution of monsoon characteristics (monsoon flow, precipitation etc).

Shortwave surface net radiation is usually determined by combining the measurement of insolation with an independent estimate of surface albedo.

The energy needed for these storms to form comes in the form of insolation, or solar radiation.