6S (radiative transfer code) - definition. What is 6S (radiative transfer code)
Diclib.com
قاموس ChatGPT
أدخل كلمة أو عبارة بأي لغة 👆
اللغة:

ترجمة وتحليل الكلمات عن طريق الذكاء الاصطناعي ChatGPT

في هذه الصفحة يمكنك الحصول على تحليل مفصل لكلمة أو عبارة باستخدام أفضل تقنيات الذكاء الاصطناعي المتوفرة اليوم:

  • كيف يتم استخدام الكلمة في اللغة
  • تردد الكلمة
  • ما إذا كانت الكلمة تستخدم في كثير من الأحيان في اللغة المنطوقة أو المكتوبة
  • خيارات الترجمة إلى الروسية أو الإسبانية، على التوالي
  • أمثلة على استخدام الكلمة (عدة عبارات مع الترجمة)
  • أصل الكلمة

%ما هو (من)٪ 1 - تعريف

ADVANCED RADIATIVE TRANSFER CODE

6S (radiative transfer code)         
6SV1 (Second Simulation of a Satellite Signal in the Solar Spectrum, Vector, version 1) is an advanced radiative transfer code designed to simulate the reflection of solar radiation by a coupled atmosphere-surface system for a wide range of atmospheric, spectral and geometrical conditions.
Radiative transfer         
ENERGY TRANSFER THROUGH A MEDIUM THROUGH EMISSION AND ABSORPTION OF ELECTROMAGNETIC RADIATION
Equation of radiative transfer; Radiative Transfer; Radiative transfer equation; Radiative transport; Radiation transport
Radiative transfer is the physical phenomenon of energy transfer in the form of electromagnetic radiation. The propagation of radiation through a medium is affected by absorption, emission, and scattering processes.
Passive daytime radiative cooling         
  • doi-access=free }}</ref>
  • Broadband PDRC emitters emit in both the solar spectrum and the infrared window (8 and 14 μm), while selective PDRC emitters only emit in the infrared window.<ref name=":54" />
  • [[Desert climate]]s have the highest radiative cooling potential due to low humidity and cloud cover.<ref name=":21" />
  • 220x220px
  • A PDRC installed on a roof in [[Kolkata]] exhibited a nearly 4.9ᵒC decrease in surface ground temperatures (with an average reduction of 2.2ᵒC).<ref name=":13" />
  • via=Elsevier Science Direct}}</ref>
  • Global map of cloud cover. Data taken from 2002 to 2015. The darker the color, the clearer the sky.
  • [[Temperate climate]]s have a moderate to high radiative cooling potential.<ref name=":21" />
  • [[Solar cell efficiency]] can be improved with PDRC application to reduce overheating and degradation of cells.<ref name="Heo 2022 Ju lee"/>
  • outgoing infrared radiation]] (shown in orange) and minimize the absorption of [[Solar Radiation]] (shown in yellow).
  • 228x228px
  • Modifying PDRCs with [[vanadium dioxide]] (pictured) can achieve temperature-based 'switching' from cooling to heating to mitigate the "overcooling" effect.<ref name=":54" />
  • Global map of average [[annual precipitation]]. The darker the color, the higher the precipitation.
MANAGEMENT STRATEGY FOR GLOBAL WARMING
Passive radiative cooling; Daytime passive radiative cooling; Daytime radiative cooling
Passive daytime radiative cooling (PDRC), passive radiative cooling (PRC), or terrestrial radiative cooling is a solar radiation management strategy that has been proposed as a solution to global warming which involves the mass installation of sky-facing surfaces on Earth that reflect heat to outer space to reverse local and global temperature increases while requiring zero energy consumption or pollution. Because all materials in nature absorb more heat during the day than at night, PDRC surfaces are designed to maximize the efficiency of both solar reflectance (in 0.

ويكيبيديا

6S (radiative transfer code)

6SV1 (Second Simulation of a Satellite Signal in the Solar Spectrum, Vector, version 1) is an advanced radiative transfer code designed to simulate the reflection of solar radiation by a coupled atmosphere-surface system for a wide range of atmospheric, spectral and geometrical conditions. It belongs to the group of procedures called Atmospheric correction for the process of removing the effects of the atmosphere on the reflectance values of images taken by satellite or airborne sensors. The code operates on the basis of an SOS (successive orders of scattering) method and accounts for the polarization of radiation in the atmosphere through the calculation of the Q and U components of the Stokes vector. It is a basic code for the calculation of look-up tables in the MODIS atmospheric correction algorithm.