Atmospheric Science and Weather Analysis Flashcards
7 cards from real CCM practice questions. Tap to flip, then mark Knew It or Still Learning — missed cards come back until you master them.
Read the first 7 Atmospheric Science and Weather Analysis flashcards as text
Which thermodynamic process describes an air parcel rising without exchanging heat with its environment?
Answer: Adiabatic
An adiabatic process involves no heat exchange with the surrounding environment, which governs unsaturated and saturated parcel ascent in the atmosphere.
The Lifted Index (LI) is computed by subtracting the temperature of a parcel lifted to 500 hPa from the environmental temperature at that level. A LI of -6°C indicates:
Answer: Extremely unstable with severe thunderstorm potential
A Lifted Index of -6°C or lower indicates extreme instability, associated with a high probability of severe thunderstorm development.
Which layer of the atmosphere is characterized by a near-constant temperature with altitude and contains the ozone layer?
Answer: Stratosphere
The stratosphere, from about 12 to 50 km altitude, has an isothermal lower portion and a warming upper portion due to ozone absorption of UV radiation.
The Bulk Richardson Number (BRN) is used in convective storm analysis primarily to assess:
Answer: The balance between buoyancy and wind shear for storm type
The BRN compares CAPE (buoyancy energy) to vertical wind shear, helping meteorologists determine whether supercells, multicells, or ordinary cells are likely to form.
In potential vorticity (PV) analysis, a stratospheric PV intrusion to the lower troposphere is associated with:
Answer: Enhanced cyclogenesis and tropopause folding
Stratospheric PV intrusions, often seen as tropopause folds, bring high-PV air into the troposphere and are strongly associated with rapid cyclogenesis.
Which radar polarimetric variable is most useful for discriminating between hail and heavy rain?
Answer: Correlation Coefficient (CC)
The Correlation Coefficient (CC) drops significantly in hail-rain mixtures because hailstones tumble and have irregular shapes, lowering the statistical consistency between horizontal and vertical pulses.
The concept of equivalent potential temperature (θe) is conserved during which atmospheric process?
Answer: Both dry and moist adiabatic processes
Equivalent potential temperature (θe) is conserved under both dry and saturated adiabatic processes, making it a powerful tracer of air mass origin and convective potential.