The Mediterranean Sea is not a factor influencing India's climate, as it is located in a different region.

The Thar Desert's continental location, far from the moderating influence of the oceans, results in extreme temperatures.

The Western Ghats, facing the Arabian Sea, receive the highest rainfall due to the orographic effect.

The temperature gradient between the heated landmass of India and the cooler Indian Ocean drives the formation of the Indian Summer Monsoon.

Blizzards are not a characteristic of the Indian Summer Monsoon, as they are associated with cold weather conditions.

ENSO can lead to altered monsoon patterns, droughts, floods, or a combination of these effects in India.

The Himalayas influence India's climate by blocking cold winds, causing orographic precipitation, and creating rain shadow regions.

Polar Climate is not found in India, as it is typically associated with high-latitude regions.

In the Northern Hemisphere, the Coriolis Effect causes cyclones to rotate counterclockwise.

Strong winds tend to disperse fog, making it less likely to form.

Droughts in India can be caused by inadequate monsoon rainfall, deforestation, overgrazing, or a combination of these factors.

Climate change is generally associated with negative impacts on agriculture, not improved yields.

The IPCC's Fifth Assessment Report covers mitigation, adaptation, and impacts of climate change.

Oxygen is not a greenhouse gas, as it does not trap heat in the atmosphere.

Climate refers to the long-term average of weather conditions, while weather describes the short-term state of the atmosphere.