Abstract
Studied the potential for forest fires near San Carlos de Rio Negro, Venezuela, one of the wetter regions of Amazonia: 3 of the communities were tall, closed-canopy forests; had closed canopies but were short in stature; and 2 had open canopies. Fine fuels reached dynamic equilibrium moisture levels (ie no further net drying given prevailing microclimate) after only 3-4 rainless days in the open-canopy and short-stature communities and after 8-10 days in the tall, closed-canopy forest types. Fine-fuel moisture content at "equilibrium' was generally twice as high in the fall, closed-canopy forest as in the other vegetation types (20% vs 10%). Surface fires were successfully started in the open-canopy and short-stature communities after 4-6 days without rain. An average of 19-27% of the available fuels were consumed by these fires. The tall, closed-canopy forest communities would not burn, even after artificially excluding rain for 41 days. The elevated relative humidities characteristic of tall, closed-canopy forests do not permit fuels to dry to the combustion point. Under current climatic conditions, fire is only possible if the relative humidity drops to 65% or below. In some open-canopy and short-stature communities, relative humidity falls below this threshold c1 day each week, on average, but in tall, closed-canopy forest such levels may occur less than 1 day each year. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 176-184 |
| Number of pages | 9 |
| Journal | Oikos |
| Volume | 53 |
| Issue number | 2 |
| DOIs | |
| State | Published - Jan 1 1988 |
All Science Journal Classification (ASJC) codes
- Ecology, Evolution, Behavior and Systematics
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