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Divergence and Vertical Motion Questions and Answers

Answer: B

An inversion suppresses vertical mixing, so emissions are confined to a shallow layer and concentrations build up, which is the mechanism behind winter smog episodes in many cities. Los Angeles owes its photochemical smog largely to the persistent subsidence inversion of the subtropical high. Long range transport requires the opposite condition of vigorous mixing and strong flow.

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62.

Assertion (A): Convergence at the surface implies ascent above.

Reason (R): Mass continuity requires that air converging into a column must leave it in some direction.

Select the correct answer from the options below.

Answer: C

With the ground preventing downward escape, converging air can only leave the column upward, so surface convergence necessarily implies ascent. The reason therefore explains the assertion completely. The same argument run in reverse gives descent above a region of surface divergence, which is why anticyclones bring clear skies. Almost every qualitative statement about cloud distribution in a synoptic system rests on this one argument.

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63.

Assertion (A): Omega is positive for ascending motion.

Reason (R): Omega is the material rate of change of pressure following the parcel.

Select the correct answer from the options below.

Answer: D

The reason gives the correct definition, and because pressure decreases upward that definition makes omega negative for ascent, so the assertion is false. The inverted sign is a frequent source of error when reading model output. Deriving the sign from the definition each time is far more reliable than trying to remember which way round the convention runs.

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64.

Assertion (A): The kinematic method gives a reliable vertical velocity over data-sparse oceans.

Reason (R): Divergence is computed as a small difference between large wind components.

Select the correct answer from the options below.

Answer: A

The reason is correct and is precisely why the assertion fails: the amplification of observational error makes the kinematic method least reliable exactly where the observations are sparsest. The omega equation, which depends on more robustly analysed fields, is the preferred alternative there. This is another instance of a true reason establishing the falsity of the assertion.

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65.

Statement I: Divergence aloft favours falling surface pressure.

Statement II: Convergence aloft favours falling surface pressure.

In the light of the above statements, choose the correct answer.

Answer: B

Surface pressure measures the weight of the overlying column, so removing mass from the top lowers it while adding mass raises it. The second statement therefore reverses the relationship. Because the upper divergence and lower convergence nearly cancel in the vertical integral, the actual tendency is a small residual, which is why forecasting surface pressure directly proved so difficult historically.

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66.

Statement I: Warm advection forces ascent in the omega equation.

Statement II: Cold advection forces ascent in the omega equation.

In the light of the above statements, choose the correct answer.

Answer: C

Warm advection forces ascent and cold advection forces descent, which is why the widespread cloud of a mid-latitude cyclone lies ahead of the warm front and the sky clears behind the cold front. The physical reasoning is that the ascent is the ageostrophic response restoring the thermal wind balance that the advection would otherwise destroy. The second statement inverts this.

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67.

Consider the following statements about omega.

1. It is negative for ascent.

2. It has units of pascals per second.

3. It can be measured directly by radiosonde.

Which of the statements given above is or are correct?

Answer: D

The first two statements are correct. Large-scale omega cannot be measured directly because the corresponding vertical velocity of about 1 centimetre per second lies far below observational accuracy, so it must be diagnosed from divergence or from the omega equation. A radiosonde measures its own ascent rate, which is governed by the balloon's buoyancy rather than by the motion of the air. Reading the definition literally, rather than recalling a formula, is the reliable route through questions of this shape. Most errors here come from carrying a result across from a neighbouring case where it does not hold.

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68.

Consider the following statements about the omega equation.

1. It is elliptic.

2. Its classical form has two forcing terms.

3. It is a prognostic equation.

Which of the statements given above is or are correct?

Answer: A

The equation is elliptic and has two classical forcing terms, but it is diagnostic rather than prognostic: it gives the vertical motion consistent with the instantaneous fields and contains no time derivative. The time derivatives were deliberately eliminated during the derivation by combining the vorticity and thermodynamic equations, which is exactly what makes the result so useful for interpreting a single analysis.

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69.

Consider the following pairs of region and vertical motion.

Ahead of a warm front - ascent

Behind a cold front - descent

Right entrance of a jet streak - ascent

Centre of an anticyclone - ascent

How many of the pairs given above are correctly matched?

Answer: B

The centre of an anticyclone is a region of subsidence, produced by frictional divergence at the surface, so the last pairing is wrong. The other three are correct. Assembling the standard regions of ascent and descent into a single mental map is one of the most practically useful things this topic offers, since it converts a chart directly into a cloud and rainfall forecast.

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70.

Consider the following pairs of method and what it uses.

Kinematic - divergence of the wind

Omega equation - vorticity and thermal advection

Adiabatic - observed temperature change

Isentropic - divergence of the wind

How many of the pairs given above are correctly matched?

Answer: C

The isentropic method uses the slope of potential temperature surfaces and the flow along them rather than the divergence of the wind, so the last pairing is wrong. The other three are correctly matched. Each method has its own error characteristics, and comparing two of them on the same case is a standard way of judging how much confidence the derived vertical motion deserves.

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