Sentence examples for by insolation from inspiring English sources

A complementary regional perspective of climate change can be assessed from internally drained lake basins, which are directly affected by insolation and precipitation balance.

The design factors were classified into three groups: (1) a factor directly affected by insolation, SHGC; (2) another group affecting heat transmission based upon the temperature difference between the indoors and the outdoors, WDI, WI, and ACR; and (3) another group affecting the effective area for heat transfer, WWR, AR, FA, CH, and PH.

Later into the afternoon, clouds will tend to bubble-up more readily across Interlagos, aided by insolation and a reasonable amount of CAPE, but any resultant showers are likely to be lighter affairs and more broadly scattered.

The entire results suggest that the reliability performance of an active distribution network can potentially be impacted by insolation variations, level of the stress of the network, and the level of penetration of PV generation.

Because of the power production capabilities of the PV generators are entirely dependent on the insolation in a particular area; the reliability of a distribution network with high PV penetration is heavily affected by insolation variations.

A new, high-precision dating method developed by the team allows better correlation of the various factors involved and puts the ice core chronologies on a stronger temporal footing, endorsing the traditional Milankovitch hypothesis, that climate variations are controlled by insolation in the northern hemisphere.

The study suggests that the variability in the ISM to the latitudinal migration of the Inter Tropical Convergence Zone was caused by insolation-driven cooling and warming events in the North Atlantic.

The land sea contrast in tropospheric temperature favored by summertime insolation is further amplified by latent heating of the monsoon rainfall that establishes deep-tropospheric monsoon circulation (e.g., Li and Yanai 1996; Webster et al. 1998; Dai et al. 2013; Wu et al. 2015; Zhang et al. 2016).

Most likely the intensity was modulated by solar insolation linked to orbital variations reflected by the large variability in δDwax and δ18Osc values.

The discrepancy between the stratospheric and mesospheric circulation can be explained by the fact that the stratospheric dynamics are mainly driven by the insolation of stratospheric ozone.

The foregoing highlights the complexity of monsoon dynamics since the last deglaciation, because the EASM was not driven simply by changing insolation, as inferred from speleothem isotope records2.