low-power lasers are a group of lasers with a power less than 250 mw and unlike high-power lasers they have no effect on tissue temperature; they produce light-dependent chemical reactions in tissues. these lasers have analgesic features with their ability to trigger reactions that reduce pain and inflammatory mediators. low-power lasers can also be used instead of needles in acupuncture to dec...

Five global monthly top-of-atmosphere (TOA) outgoing longwave radiation (OLR) products are evaluated in this study, including the derived from High-Resolution Infrared Radiation Sounder (HIRS), Clouds and Earth’s Radiant Energy System (CERES), Advanced Very High Resolution Radiometer (AVHRR), CM SAF cLoud, Albedo surface RAdiation dataset AVHRR data (CLARA), Global Water Cycle EXchanges (GEWEX)...

Present-day Arctic and Antarctic radiation budgets of the National Center for Atmospheric Research Community Climate Model version 3 (CCM3) are presented. The CCM3 simulation is from a prescribed and interannually varying sea surface temperature integration from January 1979 through August 1993. Earth Radiation Budget Experiment (ERBE) data from 1985 through 1989 are used for validation of top-...

Many important greenhouse gases (including water vapour, carbon dioxide, methane and ozone) absorb solar radiation. When gas concentrations change, this absorption exerts a radiative forcing that modifies the thermal infrared (‘longwave’) which is predominant for most (ozone being major exception). The nature of differs from longwave in several ways. For example, sign instantaneous can differ b...

[1] Tropical convective anvil clouds detrain preferentially near 200 hPa. It is argued here that this occurs because clear-sky radiative cooling decreases rapidly near 200 hPa. This rapid decline of clear-sky longwave cooling occurs because radiative emission from water vapor becomes inefficient above 200 hPa. The emission from water vapor becomes less important than the emission from CO2 becau...

Abstract. Including radiative transfer processes within the urban canopy layer into microscale climate models (UCMs) is essential to obtain realistic model results. These include interaction of buildings and vegetation with shortwave longwave radiation, thermal emission, radiation reflections. They contribute differently budget surfaces. Each process requires different computational resources p...