Global warming Hiatus

Discussion

A study was conducted in relation to the instability of mascarene highs during the global warming interval

This study showed that between 1986 and 2016 the sea surface temperature in the mascarene high balle area has increased significantly.

What is the global warming Hiatus 

This Hiatus  is the period of change in the global average temperature of the Earth's surface

The period of this interval is considered from 1998 to 2016.

During this global warming Hiatus , the rate of warming of the global surface of the Earth has been recorded. This global warming lag is called global warming stagnation or global warming slowdown b

Although sea surface temperatures have increased significantly during the global warming Hiatus 

What is Mascarene high?

Mascarene high is semi permanent subtropical high pressure zone. It is also called Indian Ocean Subtropical Tropical Anything.

This subtropical high pressure area is located near Mascarene Vip in the south Indian Ocean between 20 ° to 35 ° south latitude and 40 ° to 90 ° east longitude.

Mascarene Islands are a group of islands in the Indian Ocean east of Madagascar from where the cross equatorial wind's flows towards India. Mascarene high also affects patterns in weather in Africa and Australia.

Also Mascarene high helps in differential hemispheric circulation between the Indian Ocean in the south and the subcontinent terrain in the north

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Effect of Mascarene high

Mascarene high is an important component of the southwest monsoon. Due to this, there is rainfall in the Indian subcontinent.

East Asia receives more than 80% of annual rainfall due to Mascarene high. I Screen high intensity in southern Indian Ocean has decreased due to global warming interval

The pressure gradient between Mascarene High and Indian Territory has declined due to increase in sea surface temperature due to global warming interval.

The intensity of the cross equatorial wind's flowing downstream over the western Indian Ocean due to a drop in pressure gradient is eliminated.

Which has an impact on the arrival of monsoon in the Indian subcontinent and rainfall in East Asia.

As a result, there is a change in the timing and pattern of arrival of monsoon, its direct effect is studying on the yield of agriculture.