1992
DOI: 10.1080/00221349208979845
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The Caribbean Sugar Bowl: A Case Study of “Human-Environment Interaction”

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Cited by 3 publications
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“…No long‐term climate data exist for the Dominican highlands. An isohyet map for the country as a whole indicates annual precipitation in JPRNP of ∼1000–1600 mm (Martinson 1992), but these values derive from interpolation from mid‐elevation stations, and may be tenuous owing to the spatial variability of mountain climate where elevations approach or exceed the TWI. Rainfall in the highlands is strongly seasonal; little rain falls between January and March, and subfreezing overnight temperatures and frost are common during that time.…”
Section: Methodsmentioning
confidence: 99%
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“…No long‐term climate data exist for the Dominican highlands. An isohyet map for the country as a whole indicates annual precipitation in JPRNP of ∼1000–1600 mm (Martinson 1992), but these values derive from interpolation from mid‐elevation stations, and may be tenuous owing to the spatial variability of mountain climate where elevations approach or exceed the TWI. Rainfall in the highlands is strongly seasonal; little rain falls between January and March, and subfreezing overnight temperatures and frost are common during that time.…”
Section: Methodsmentioning
confidence: 99%
“…No long-term climate data exist for the Dominican highlands. An isohyet map for the country as a whole indicates annual precipitation in JPRNP of ∼1000-1600 mm (Martinson 1992), but these values derive from interpolation from mid-elevation stations, (Horn et al 2001). Years since fire are reported with respect to the time of data collection (1999).…”
Section: Methodsmentioning
confidence: 99%