In the Mediterranean forest area of Israel, fires increase runoff and
sediment yield rates relative to undisturbed forested land. The Septem
ber 1989 fire covered an area of 4 km(2) in the main recreation area o
f Mount Carmel, a typical Mediterranean forest area. The lithology is
chalk and limestone, and about 40% of the burnt area has steep slopes,
exceeding 30%. Three study plots were established in burnt and unburn
t areas. Plots were located on 100-300 m(2) areas with different slope
exposures. Runoff and sediments were collected after each storm by a
collector system. A hydrometric station was established, draining an a
rea of 1 km(2) in the burnt zone. Rainfall was measured by two recorde
rs and several rain gauges at the experimental sites. In the first rai
nfall season after the fire, runoff and sediment yield were 500 and 10
0,000 times higher respectively in the burnt areas. Rainfall intensity
is a dominant factor in runoff and sediment yield rates. In the measu
red basin, total runoff in the first year was 1.6%. Revegetation recov
ery of the area was rapid, as shown by the results from the second sea
son: runoff decreased by one order of magnitude, from an average of 10
mm to 1.5 mm; sediment yield decreased by two orders of magnitude, fr
om 1200 g m(-2) to 10 g m(-2). The third season 1991/1992, was an exce
ptionally rainy year and therefore runoff and sediment yield increased
, but to less than in the first year. Runoff and sediment yield are re
lated to vegetation cover, rainfall intensity, soil properties, slope
steepness and exposure and fire intensity. Logging activities after fi
re increase sediment yields. Through its effects on vegetation cover a
nd soil, fire severity increases the potential for erosion. (C) 1998 E
lsevier Science B.V. All rights reserved.