ट्रोपोपॉज इसके अंग्रेजी अर्थ का उदाहरण

\end{align}Where the first equation represents the requirement for radiative equilibrium at the tropopause and the second equation represents how much water vapor is present at the tropopause.

The Simpson-Nakajima limit builds off of the derivation of the Komabayashi-Ingersoll limit by assuming a convective troposphere with a surface temperature and surface pressure that determines the optical depth and outgoing longwave radiation at the tropopause.

At that value the Stefan-Boltzmann feedback breaks down because the tropospheric temperature required to maintain the Komabayashi-Ingersoll OLR value results in a water vapor optical depth that blocks the OLR needed to cool the tropopause.

This approach focuses on the balance between the outgoing longwave radiation at the tropopause,F^\uparrow_\text{IRtop}, and the optical depth of water vapor, \tau_\text{tp}, in the tropopause, which is determined by the temperature and pressure at the tropopause according to the saturation vapor pressure.

ट्रोपोपॉज हिंदी उपयोग और उदाहरण

""ये वायुमण्डल में निचले स्तर से लेकर ट्रोपोपॉज़ तक आकार धारण करते हैं।