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the claim

Monsoons are primarily caused by seasonal temperature differences between landmasses and oceans

the verdict
SUPPORTED
the evidence backs this
Recorded sources
4 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Is it true that monsoons are primarily caused by seasonal temperature differences between landmasses and oceans?

Yes. Monsoons are fundamentally driven by the seasonal differential heating between landmasses and oceans, creating the thermal contrasts that power large-scale atmospheric circulation and precipitation.

Verdict: SUPPORTED · 4 sources for, 0 against · Last checked

The analysis

The retrieved papers consistently emphasize land-sea thermal contrast as a primary driver, mechanism, and index for monsoon systems across different regions, supporting the claim without any contradictory evidence regarding this foundational meteorological principle.

Evidence for · 4
Understanding the Predictability of East Asian Summer Monsoon from the Reproduction of Land–Sea Thermal Contrast Change in AMIP-Type Simulation
2010
Demonstrates that land-sea thermal contrast is central to reproducing and predicting East Asian summer monsoon circulation.
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Zhou, T. & Zou, L. (2010). Understanding the Predictability of East Asian Summer Monsoon from the Reproduction of Land–Sea Thermal Contrast Change in AMIP-Type Simulation. doi.org. https://doi.org/10.1175/2010jcli3546.1

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More for · 3
A monsoon-like Southwest Australian circulation and its relation with rainfall in Southwest Western Australia
2010
Identifies land-sea thermal contrast as a primary characteristic and driver of monsoon-like circulation in southwest Western Australia.
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Feng, J., Li, J., & Li, Y. (2010). A monsoon-like Southwest Australian circulation and its relation with rainfall in Southwest Western Australia. doi.org. https://doi.org/10.1175/2009JCLI2837.1

Role of the land‐sea thermal contrast in the interannual modulation of the North American Monsoon
2009
Shows that land-sea thermal contrast serves as a principal driving mechanism for North American Monsoon onset variability.
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Turrent, C. & Cavazos, T. (2009). Role of the land‐sea thermal contrast in the interannual modulation of the North American Monsoon. doi.org. https://doi.org/10.1029/2008gl036299

Delayed response of the onset of the summer monsoon over the Bay of Bengal to land–sea thermal contrast
2023
Highlights how land-sea thermal contrasts across meridional, zonal, and cross-equatorial directions drive the onset of the Bay of Bengal summer monsoon.
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Sun, W., Wu, G., Liu, Y., Mao, J., Zhuang, M., & Liu, X. (2023). Delayed response of the onset of the summer monsoon over the Bay of Bengal to land–sea thermal contrast. doi.org. https://doi.org/10.1175/jcli-d-22-0478.1

What does the evidence say?

The retrieved papers consistently emphasize land-sea thermal contrast as a primary driver, mechanism, and index for monsoon systems across different regions, supporting the claim without any contradictory evidence regarding this foundational meteorological principle.

Receipt History
first checked04 Aug 2026
judged → SUPPORTED · 8704 Aug 2026
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