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The electron temperature is determined by the balance of heating through photoelectrons that are created by the solar EUV irradiance, cooling through collisions with neutrals and ions, and heat conduction along magnetic field lines.
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In this model, ENSO reacts to solar irradiance due to a zonal asymmetry in the response of the tropical pacific: a heating due to higher irradiance would cool the East Pacific, inducing a La Niña-like climatic system.
The new record temperature in 2010 is particularly meaningful because it occurs when the recent minimum of solar irradiance is having its maximum cooling effect.
Cultures were maintained in glass 250 mL flasks in a cabinet at a constant temperature of 26°C and under continuous irradiance of cool white light at an intensity of 15 μmol photon m-2 s-1.
In addition, optimal sizes for the absorption subsystem should be designed according to the different minimum product cost flow rates or the lowest relative cost difference, and this difference is sensitive to the local mean solar irradiance but weakly relies on the cooling demand.
Previous studies have shown that a large proportion of the net energy demand of an office building is related to window heat loss and cooling demands induced by solar irradiance.
The multiple regression fit has also enabled the relative roles of solar irradiance and geomagnetic processes in driving the NO cooling to be determined.
Irradiance brings solar heat gains that transfer to building cooling load, while illuminance provides a luminous environment and affects artificial lighting system at the same time.
Furthermore, the effects of direct normal irradiance level, ambient wind speed, seawater temperature, various cool side cooling options for the thermoelectric generator on the system performance are investigated.
The observed changes in thermospheric cooling correlate well with changes in solar ultraviolet irradiance and geomagnetic activity during the prior maximum conditions.
Triggers for cold anomalies are linked to variable combinations of freshwater pulses, low total solar irradiance, explosive and effusive volcanism, and internal modes of climate variability, with cooling likely sustained by ocean/sea-ice feedbacks.
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