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Latin America; in English (pdf) - Transboundary Freshwater Dispute ...

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BIOPHYSICAL PARAMETERS<br />

A B<br />

Map 1 (A) Climate Regions.<br />

Köeppen climate zones based on a 0.5 decimal degree grid by Leemans and Cramer (1991) published by the International Institute for Applied Systems Analysis (IIASA). The<br />

Köeppen system <strong>in</strong>tegrates IIASA average monthly ra<strong>in</strong>fall total and average monthly temperature, <strong>in</strong> most cases averaged from 1961–1990, to yield five base climate types: tropical, dry, temperate, cold,<br />

and polar. Each primary type is divided <strong>in</strong>to sub-classes based ma<strong>in</strong>ly on the distribution of ra<strong>in</strong>fall and temperature throughout the year. Not all classes may be represented at the cont<strong>in</strong>ental level.<br />

(B) Average Annual Runoff<br />

unoff. Fekete et al. (1999) produced composite runoff fields by access<strong>in</strong>g GRDC discharge data, select<strong>in</strong>g significant global gaug<strong>in</strong>g stations, and geo -register<strong>in</strong>g the discharge<br />

<strong>in</strong>formation to locations on a simulated topological network. This dataset was deemed accurate for presentation with a 0.5 decimal degree grid. Summary statistics based on the runoff dataset, such as<br />

those used for projected water stress (human <strong>in</strong>dicators), may not be considered accurate for bas<strong>in</strong>s with an area less than approximately 25,000 km 2 .<br />

80 — Hydropolitical Vulnerability and Resilience along International Waters: <strong>Lat<strong>in</strong></strong> <strong>America</strong> and the Caribbean

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