Climatic Controls

Along with nearness to sea wind direction and relief also decide rainfall. Rain shadow and dry winds can reduce rainfall.

Many physical and atmospheric controls work together in India. Therefore great climatic diversity is found.

As altitude increases temperature decreases and vegetation belts may change. This is clearly seen in mountain areas.

Latitude changes the angle of sun rays. Therefore temperature generally decreases away from the Equator.

A cold current can cool the air near the coast. Remember the effect of ocean currents on coastal temperature.

Wind brings characteristics of its source region. Therefore marine or land sources can change climate.

In complex regions several controls act together. Therefore sea, altitude and relief should be studied together.

Climate is controlled by more than one factor, so the two conditions in the question must be considered together. A high place is generally cooler because temperature usually decreases with increasing altitude. A leeward place lies on the sheltered side of a mountain range, where descending air is often drier and rainfall is lower than on the windward side. Together, these controls can produce cool and relatively dry conditions.

Option A is correct because it combines the likely effects of altitude and leeward position. The word “may” is important: it expresses a possible tendency, not an unchangeable rule. The other options claim impossible or unrelated results. Good climate analysis considers several controls instead of allowing one factor to cancel or ignore the other.

Both are linked with marine influence but their roles differ. Distance gives broad coastal influence and currents change specific coastal temperature.

The effect of climatic controls is generally understood through long-term and regional patterns. One event may be weather.

Moist sea winds can rise over altitude, cool and give rainfall. This is a combined effect of relief and wind.

Low altitude and tropical latitude can increase temperature. Study altitude effect with other controls.

In India the monsoon is affected by sea, pressure-wind system, Himalaya and relief. This is the complexity of climate.

The sea changes temperature slowly, reducing day-night difference. This is clear in coastal areas.

Distance from sea can increase temperature extremes and dry winds can reduce moisture. This is effect of combined controls.

When differences occur at the same latitude other controls must be examined. This is a good example of combined climate analysis.

Climatic controls such as latitude, altitude, distance from sea, wind and relief together form regional climate. Understand them as causes.

In complex geographic location sea, altitude, relief and winds work together. Therefore combined analysis is necessary.

Cold current and altitude can reduce temperature while leeward position can reduce rainfall. Understand combined controls together.

Climate is formed by combined effects of latitude, altitude, sea, wind and relief. Therefore conclude only after checking many controls.