The main aspects of the physical environment which determine the biomes and ecoregions of Zambia are: climate, specifically rainfall amount, length of the dry season, and temperature, which is related to elevation; and soils and bushfires.
Zambia experiences good rainfall, with extremes of 500 to 1400 mm (most areas fall into the range 700 to ) in a distinct rainy season of four to six months centred on January, when the moist Intertropical Convergence Zone is over the country.
Along the banks of permanent rivers and in the spray of waterfalls are evergreen thickets similar in character to tropical rainforest, relics of a wetter past.
For animals, adaptations to drought are seen in migration and breeding patterns, as well as the ability, found in rodents and reptiles especially, to obtain water requirements from food without the need to drink.
The elevation of the great central African plateau on which Zambia is located, typically between 1000 and 1300 metres, modifies temperatures, which are lower than for coastal areas at the same latitude, and pleasant for much of the year.
Frost only occurs on a few days in winter on the highest exposed hills, or more widely in the lower humidity areas of the southern half of the country.
Bush fires range across most of the country in the later dry season, escaping from "chitemene cultivation" and caused by villagers burning off crop residue or hunting, as well as by lightning strikes.
Prevailing winds are not usually very strong and a lack of a great deal of dry fuel on the ground (since most areas are burnt annually it does not build up) means that the fires are not as devastating as in countries such as Australia and the south-western USA.
However, except in the case of the last ecoregion listed, even where the canopy is extensive, at ground level the woodland is relatively open, affording quite easy passage by animals and people.
It is well adapted to hot dry areas on sandy soils, and forms extensive forests which have been over-exploited by commercial timber production over the past 75 years, in: These are the most extensive non-floodplain grasslands in Zambia, covering about 5% of the country in the west, and support large herds of wildebeest which migrate between western Zambia and Angola.
As a country with very distinct rainy and dry seasons, with a high rainfall in the former, and having a fairly flat topography, Zambian rivers and low-lying areas are prone to flooding, and there are extensive permanent swamps.
Plants, animals and people have evolved to this cycle which in Zambia has been fairly reliable, and it brings a number of ecological advantages which promote biodiversity.
The role of termites in building mounds which remain above most of the flood is important as this provides habitats for plants less tolerant of getting waterlogged, as well as safe breeding sites for birds and some animals.
This ecoregion is made up of grassland and shrubland, with a great variety of orchids and wildflowers on exposed hills, with forest in narrow valleys and small depressions.