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Sunshine and rain are the two things most people mean by the weather, but they are usually mapped one at a time. I combine them in a bivariate map of the world's land, using the CRU CL 2.0 climatology for 1961 to 1990 on a 10 arc-minute grid: 566,262 cells with both mean monthly sunshine, which I convert from a percentage of possible sunshine to hours using the astronomical day length, and mean monthly precipitation. Classed by terciles of land area, the two measures are far from independent (Spearman's rho = -0.24). The sunny and dry corner holds 21.0% of the land and the sunny and wet corner only 3.0%, against the 11.1% expected if they were unrelated. The dull and dry corner, 7.3% of the land, is mostly subarctic, but among 573 cities of a million people or more it contains only Lima, Callao and Trujillo on the desert coast of Peru. The United Kingdom sits at the dull end of the world: its sunniest cell gets 1,774 hours a year, and 84% of the world's land gets more; only three of 156 countries are duller on average. A comparison with WorldClim 2.1 precipitation shows close agreement for rain (Pearson's r = 0.977), but no independent check is available for sunshine, which rests on far fewer stations. An interactive version lets readers re-cut the classes by month and by break, search 34,167 places, and find each place's closest weather twins. Interactive version: https://tristan-hotham.github.io/sun-and-rain/. Data and code: https://github.com/Tristan-Hotham/sun-and-rain. Blog post: https://blog.tristanhotham.com/2026/10/28/sun-and-rain/. Text, figures and derived data: CC BY 4.0; code: MIT. Climate data: CRU CL 2.0, Climatic Research Unit, University of East Anglia, New et al. (2002), shared as derived products with citation. Places: GeoNames (CC BY 4.0). Country outlines: Natural Earth (public domain). WorldClim 2.1 is used for summary statistics only and is not redistributed.
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Tristan Hotham (2026) studied this question.
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