---
title: "Tibetan Plateau Heating and the Monsoon — Definition"
description: "Tibetan Plateau heating warms the mid-troposphere over Tibet, generating the Tibetan anticyclone and the easterly jet that intensify the Indian summer monsoon."
url: "https://modeldiplomat.com/learn/glossary/tibetan-plateau-heating"
---

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Model Diplomat Research Team · Last reviewed June 22, 2026

TL;DR

- Tibetan Plateau heating is the seasonal warming of the elevated Tibetan landmass that drives a mid-tropospheric high and intensifies the South Asian summer monsoon circulation.
- How does Tibetan Plateau heating differ from the classical land-sea thermal contrast theory of the monsoon?
- What is the Tropical Easterly Jet's connection to the plateau?
- Why did Boos and Kuang's 2010 study challenge the plateau heating theory?
- How does Himalayan snow cover relate to monsoon prediction?

[Civil Service & Diplomatic Exams](https://modeldiplomat.com/learn/civil-services/glossary)Updated June 22, 2026

Tibetan Plateau heating is the seasonal warming of the elevated Tibetan landmass that drives a mid-tropospheric high and intensifies the South Asian summer monsoon circulation.

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In June 2023 the India Meteorological Department cited the northward shift of the subtropical westerly jet past the Tibetan Plateau among the factors confirming monsoon onset over Kerala on 8 June.

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