Rivers and streams occupied by anadromous Atlantic salmon (Salmo salar) occ
ur across a diverse array of landscapes. This article describes the general
ecology of these rivers and streams, including many of the physical and bi
ological variables that are important characteristics of all lotic systems.
For analytical purposes, the geographic range of Atlantic salmon rivers is
divided into dye regions, based on geomorphology and climate. The physical
habitat available to anadromous Atlantic salmon is diverse. The geology va
ries from granitic bedrock to volcanic and glacial substrates, which influe
nce a broad array of other ecological variables, ranging from water chemist
ry to catchment morphology (e.g., river length). Flood regimes and system h
ydrology are dependent, as expected, on climate. Many of the catchments rec
eive substantial precipitation in the form of snow; rivers in four of the f
ive regions experience primarily spring freshets. Aquatic temperatures are
also variable, representing close to the full range of thermal tolerance of
S, salar, with lows just above 0 degrees C in the northernmost latitudes t
o summer highs in western Europe approaching 25 degrees C. Most rivers are
best characterized as oligotrophic with relatively low annual primary produ
ctivity. However, physical factors such as availability of suitable spawnin
g and rearing habitat, as well as aquatic temperature and flow regimes, may
drive anadromous productivity. In general, most of the rivers have been mo
dified by flow regulation and many suffer from impacts related to other ant
hropogenic disturbances, principally riparian forest clearing for agricultu
re, forestry, and urban development. We conclude that the rivers and stream
s occupied by anadromous Atlantic salmon are diverse across the species' ra
nge and have been heavily impacted by anthropogenic disturbances.