UV variability in Moscow according to long-term UV measurements and reconstruction model

Girit’te çıkan bu isyanlara, Avrupa devletleri çıkarları gere i ilgisiz kalmamı tır. ttihat ve Terakki Cemiyeti’nin yayın organı olan Osmanlı Gazetesi de

The well- predicted aerosol quantities, such as aerosol number, mass composition and optical properties, and the inclusion of full aerosol-cloud couplings lead to

Annual totals of UV radiation derived from reconstructed daily UV values reflect in- terannual variations and long-term patterns that are compatible with variabilities and changes

fire aerosol radiative effect (RE) at TOA, radiative effects due to aerosol–radiation interactions (REari), due to aerosol–cloud interactions (REaci), surface-albedo changes (REsac)

The cloud optical thickness and the droplet e ff ective radius are retrieved from spectral radiance data in nadir and and from hyperspectral radiances in a 40 ◦ field of view..

measured from Terra are also compared to LBLMS simulations in cloudy conditions using retrieved cloud optical depth and e ff ective radius from MODIS. Three case stud- ies are

di ff erences due to cloud parameterization schemes, in CTL and MAC, the other is the influence of aerosol activation and associated cloud particle numbers and sizes; how- ever, the

Indeed, from this model, we can simulate the lamp current, voltage and power as. well as the response in bacteriological attack according to UV