Meso-scale Atmospheric Motion Scale Identification
Atmospheric motions are categorized by their characteristic horizontal scale lengths. Meso-scale motions represent a specific category within this classification.
Meso-scale phenomena are larger than micro-scale events (like turbulence) but smaller than large-scale synoptic systems (like major low-pressure areas).
The established range for meso-scale atmospheric motions spans horizontally from approximately 30 km to 400 km.
Key examples of meso-scale phenomena include:
- Individual thunderstorms
- Mesoscale convective systems (MCSs)
- Land and sea breezes
- Mountain waves
Understanding this scale is vital for predicting localized and regional weather patterns.
Other scales for context include:
- Microscale: Less than 1 km
- Synoptic scale: Greater than 400 km (often thousands of km)
Important Questions from Atmosphere
- What is atmospheric window?
- Which one of the following gas was not released through volcanoes around 4 billion years ago?
Absolute humidity in atmosphere at $ 10^\circ $ is $5.0$ g/m$^3$ and maximum amount of water air can hold at same temperature is $ 10$ g m$^3$. What will be the relative humidity at the same temperature?
- The change of atmospheric air temperature with altitude is _____
- Assertion (A) : Warmth of sun’s rays is advantageous during evening time.
Reason (R) : Evening air contains moisture which absorbs the heat and allows the light.
Select the most appropriate option :
