
Photo Credit: Onofre Quezada
Scientific Frontline: Extended "At a Glance" Summary: Shifting Climate in Caribbean Tropical Forests
The Core Concept: Despite the conventional assumption that tropical ecosystems possess stable climates, recent data reveals that these regions are experiencing rapid, significant increases in extreme temperature and localized precipitation events. This destabilization is driven by global climate change and is currently affecting even highly protected areas.
Key Distinction/Mechanism: Hydroclimatic responses to global warming in the tropics are not uniform; they are highly localized and can diverge dramatically over short geographic distances. For example, while two closely located Caribbean sites both experienced a severe increase in extreme heat days, one site became significantly wetter with heavy rainfall, while the other experienced prolonged dry extremes.
Origin/History: Researchers identified a decadal warming trend of 0.29°C by analyzing continuous monitoring data collected from 1975 to 2024 in Puerto Rico, and from 1983 to 2024 in Costa Rica. By 2024, the frequency of extreme heat days at these sites had quadrupled compared to historical baselines.
Major Frameworks/Components:
- Hydroclimatic Monitoring: The continuous assessment of air temperature, water temperature, precipitation, and stream water levels using automatic and manual sensors.
- Extreme Event Frequency: The statistical tracking of environmental events that exceed the 95th, 97th, and 99th percentiles for heat and precipitation.
- Localized Divergence: The phenomenon of geographically proximate ecosystems exhibiting contrasting climate impacts, such as wet extremes versus dry extremes.
- The El Niño Southern Oscillation (ENSO): The evaluation of how broader climatic phases, such as La Niña, influence local temperature variations in specific regions.

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