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RADIATIVE - translation to arabic
RADIATIVE
الفعل
اِسْتَهَلَّ الوَجْهُ ; تَهَلَّلَ
heat radiation
![Thermal radiation in visible light can be seen on this hot metalwork. Its emission in the [[infrared]] is invisible to the human eye. [[Infrared cameras]] are capable of capturing this infrared emission (see [[Thermography]]).](https://commons.wikimedia.org/wiki/Special:FilePath/Hot metalwork.jpg?width=200 "Thermal radiation in visible light can be seen on this hot metalwork. Its emission in the [[infrared]] is invisible to the human eye. [[Infrared cameras]] are capable of capturing this infrared emission (see [[Thermography]]).")
![National Research Council]], near [[Ottawa]], [[Ontario]], Canada](https://commons.wikimedia.org/wiki/Special:FilePath/Radiant heat panel nrc ottawa.jpg?width=200 "National Research Council]], near [[Ottawa]], [[Ontario]], Canada")
ELECTROMAGNETIC RADIATION GENERATED BY THE THERMAL MOTION OF CHARGED PARTICLES IN MATTER
Radiant heat; Heat radiator; Thermal radiator; Thermal Radiation; Thermal light; Heat radiation; Radiative heat transfer; Radiation of heat; Thermal emission; Radiation heat transfer; Radiation properties
إشعاع الحرارة ، الحرارة الإشعاعية
thermal radiation
ELECTROMAGNETIC RADIATION GENERATED BY THE THERMAL MOTION OF CHARGED PARTICLES IN MATTER
Radiant heat; Heat radiator; Thermal radiator; Thermal Radiation; Thermal light; Heat radiation; Radiative heat transfer; Radiation of heat; Thermal emission; Radiation heat transfer; Radiation properties
إشعاع حرارى ، حرارة مشعة
Examples of use of RADIATIVE
1. Most of the increase in radiative forcing measured since 1''0 is due to CO2, which now accounts for about 62 percent of the radiative forcing by all long–lived greenhouse gases.
2. Most of the increase in radiative forcing measured since 1''0 is due to carbon dioxide, which now accounts for about 62 percent of the radiative forcing by all long–lived greenhouse gases.
3. Positive radiative forcing tends to warm the surface of the Earth, and negative forcing tends to cool the surface.
4. Its focus is on the crucial role of clouds and their influence on radiative feedback processes in the atmosphere.
5. Radiative forcing is the change in the balance between solar radiation coming into the atmosphere and Earth‘s radiation going out.