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Suriname

1 city

Climate overview

Suriname (approximately 163,820 km²) occupies the northeastern shoulder of South America between 1°50'–6°N, bordered by the Atlantic Ocean to the north (386 km coastline), French Guiana to the east (Maroni/Marowijne River boundary), Guyana to the west (Corantijn River boundary), and Brazil to the south, encompassing a quintessential tropical rainforest climate across 90% of its interior.

The country divides into distinct zones: the densely populated low-lying coastal plain where most of the population lives, including capital Paramaribo; a savanna belt; and the vast forested interior (approximately 80% of national territory) rising to about 1,230–1,290 m at Julianatop in the Wilhelmina Mountains.

The climate is predominantly Köppen Af (tropical rainforest) with mean annual temperatures of 27°C showing minimal seasonal variation, though the interior experiences slight cooling at higher elevations. Annual precipitation averages 2,200 mm on the coast and is higher in parts of the interior, distributed across two wet seasons (roughly November–February and April–August) separated by two dry periods, though the interior remains humid year-round.

The northeastern trade winds moderate coastal temperatures but bring persistent humidity; the Intertropical Convergence Zone (ITCZ) seasonal migration governs rainfall patterns; interior rivers including the Suriname, Saramacca, Coppename, and Marowijne drain north through dense rainforest, creating flood vulnerability when seasonal rains coincide with spring tides.

Paramaribo (coastal, near sea level) sees highs of about 29°C in January and 31°C in July with 2,200 mm annual rainfall, experiencing oppressive year-round humidity with heat indices regularly exceeding 35°C, rarely dropping below 22°C at night.

The severe May 2006 floods inundated about 30,000 km² of the interior, including 157 villages, and affected up to 25,000 people in areas such as Pokigron, Tapanahony, Lawa and Marowijne, mostly in Indigenous and Maroon settlements.

Lelydorp, south of Paramaribo, Brokopondo (interior, near the reservoir) and Stoelmanseiland (deep interior, on the French Guiana border) share similarly warm, wet conditions, the dense canopy buffering temperature extremes inland.

Sea-level rise threatens most of Suriname's population clustered on the low-lying coastal plain; Paramaribo and coastal agriculture are increasingly vulnerable to storm surge and saltwater intrusion into aquifers and rice fields.

Recent droughts have stressed hydropower generation at the Brokopondo reservoir (critical for national electricity). Bauxite mining in the savanna belt stripped vegetation and compacted soils, which can accelerate runoff.

Comparing the last decade against the 1940–1970 baseline, mean temperatures across these cities have risen by about 1.3°C.

Sources:Climate Change Knowledge Portal: SurinameIPCC AR6 WG1 Chapter 12: Climate Change Information for Regional Impact and for Risk AssessmentGeography of Suriname2006 Suriname floodsSea Level Rise and Coastal Vulnerability in Suriname

How the climate has shifted in Suriname

Average across 1 city with full ERA5 coverage: 1940–1970 baseline vs the last decade (2016–2025).

+1.3°Cwarmer than the 1940–1970 baseline
Annual mean temperature
25.7°C→27.0°C
Days above 30°C per year
147 days→259 days+112
Frost days per year
0 days→0 days+0
Tropical nights (≥20°C) per year
365 nights→365 nights+0

What's unusual right now

From a snapshot of the world's largest cities updated each hour. Today's mean temperature compared with each city's long-term average for the same calendar date (ERA5 climatology, 1940 onward). Last 30 days uses each city's rolling daily-mean vs its monthly average. Not a global ranking.

Last 30 days vs averagerolling 30-day mean

Warmer than usual

Warmest in Suriname right now

Coolest in Suriname right now

From a snapshot of the world's largest cities updated each hour. Not a global ranking.

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