Forests
in boreal and temperate zones are a major stabilizing component
of natural landscapes. Forests protect and regulate the environment,
clean both the atmosphere and water, deliver about 5000 different
goods to sustain local populations and the national economy, and
finally serve as a vitally important prerequisite of human life.
Due to its large scale (23% of the global forested area) and a
number of important inherent features, Russian forests are a phenomenon
of the global commons. Stretching for eleven time zones from west
to east and for several thousands of kilometers from north to south,
the Russian forest zone comprises diverse ecosystems and landscapes,
plants and animals.
There are hundreds of definitions of forests
globally. From an ecosystem point of view, a forest is a vegetation
type and part of a larger system of trees, shrubs, herbs
and other plants (mosses, lichens) including animals and microorganisms
which all interrelate in their development and interact with each
other and the environment.
Technical definitions of a forest are usually based on quantitative
indicators describing a stand (a grouping of trees based on some
classification system). The Russian definition (which is used everywhere
in this CD) defines a forest, or forested area (due to the current
Forest Inventory Manual), as territories covered by trees with
relative stocking (the indicator which on average correlates with
canopy closure) of 0.35 and greater for young forests, and 0.25
and greater for older age categories.
Forests are an important part of the biosphere, and the source of many resources:
industrial, food, fodder, and medicinal. As a rather stable dynamic biological
system, forests are slowly evolving over time and space in response to environmental
changes. At the same time, the forest influences the environment. The forest,
as a self-regulating system, tends to reach dynamic equilibrium by exchanging
matter and energy with the environment. This process is performed through the
mechanisms of natural selection and is accompanied by the evolution of all components
of forest biogeocenosis.
Forests are known to substantially impact regional climates.
Increasing of forested area by 10% in the steppe region of European Russia has
lead to a growth in annual precipitation of 10-15 millimeters (mm) on average.
Forests substantially impact the water balance of the territory, regulate runoff,
and finally form the hydrological regime of landscapes. The water-regulating
role of forests consists of reducing surface runoff while increasing underground
runoff. Forest shelterbelts protect soils against erosion and smooth unfavorable
climatic impacts. The spiritual, cultural, and aesthetic aspects of the forest
are also of great importance.
Forests are a major land use-land cover type in Russia. Forest land (territories
identified for forests and forestry) comprise 51.6% of the country’s
land. Closed forests (forested areas) cover 776 million ha or 45.4% of the
total land area. Of the total forested area, in 2003, 18% of forests were classified
as protective forests, 7.6% were destined mostly for ecological services with
prohibited or restricted industrial logging, and 69.4% were basically destined
for timber extraction (the new Forest Code introduced categories of protective,
exploitable and reserved forests). Due to large areas of protective and low productive
forests, only 45% of Russian forests are classified as forests available for
industrial logging. The absolute majority (~ 95%) of Russian forests are in the
boreal zone that defines the prevalence of coniferous species (70%). Major dominant
tree species include larch (35% of all forested area), pine (16%), spruce and
fir (12.5%) and Stone pine (Russian cedar) – 5.6%. Deciduous
broadleaved forests comprise 17%, mostly secondary birch and aspen. Relatively
small areas (2.5%) are covered by valuable hard wood deciduous forests dominated
by oak, ash-tree, beech etc. The rest (~10%) is mostly represented by dwarf
pine and other shrubs, in regions where tall trees are not able to grow due
to severe climatic conditions. The growing stock of Russian forests (i.e., the
total amount of stem wood of all living trees) was 88.3 billion m3 in 2003.
Major Land
Categories and Forest Management Activities in Forest Fund of
MNR in 2005
Forests occur in all geographic zones from the
sub-Arctic to the subtropics in Russia (Table 1). The major factors
that influence the distribution, species composition, structure
and productivity of forests are temperature, precipitation, continentality
and aridity of climate, land-use/land cover change and natural
and human-induced disturbances. The impact of climate is revealed
in geographical and altitudinal zonality of forests. Arctic and
sub-Arctic deserts are treeless. Relatively small forested areas
(about 5 million ha) penetrate the Arctic coast of European Russia
and the tundra zone of Siberia and the Far East along river valleys.
Forests grow up to 72 deg 30' N (the Khatanga River Basin
north of Krasnoyarsky Kray) – this comprises the most northward
forested area over the globe. Southward of the tundra, a mixture
of low productive forests and treeless territories dominate,
and are represented by wetlands and tundras with dwarf vegetation,
shrubs, grasses, mosses and lichens. Light coniferous forests,
mostly dominated by larch, cover about 145 million ha in the forest
tundra zone, along with the sparse and northern taiga. Stand density
and productivity of forest increase from north to south.
Table 1. Distribution of areas of Russian forests by bioclimatic zones and dominant
species, x 10^6 ha, based on data of SFA-1993. Source: IIASA Forestry Program
Zone 1 |
Distribution of
forested areas (FA) by dominant species, x 10^6 ha |
UFA 2 |
FL 2 |
pine |
spruce |
fir |
larch |
cedar |
birch |
aspen |
other |
shrub |
total |
T |
0.1 |
0.0 |
0.0 |
0.2 |
0.0 |
0.5 |
0.0 |
0.0 |
3.0 |
3.8 |
3.5 |
7.3 |
FT |
21.8 |
23.9 |
0.0 |
71.9 |
7.3 |
7.7 |
0.3 |
0.1 |
8.1 |
141.2 |
55.8 |
197.0 |
MT |
60.4 |
43.1 |
11.1 |
191.0 |
29.9 |
46.7 |
7.9 |
10.3 |
54.7 |
455.0 |
34.5 |
489.5 |
S T |
41.2 |
17.7 |
5.2 |
7.6 |
3.2 |
38.4 |
10.7 |
2.3 |
0.1 |
126.5 |
21.8 |
148.3 |
TF |
3.1 |
0.2 |
0.1 |
0.0 |
2.6 |
4.4 |
2.4 |
14.4 |
0.2 |
27.4 |
5.7 |
33.1 |
S |
2.1 |
0.0 |
0.0 |
0.0 |
0.1 |
2.9 |
1.1 |
1.8 |
0.4 |
8.3 |
1.6 |
9.9 |
SD |
0.1 |
0.0 |
0.0 |
0.0 |
0.0 |
0.3 |
0.0 |
0.7 |
0.2 |
1.3 |
0.1 |
1.4 |
Total |
128.8 |
84.8 |
16.4 |
270.0 |
43.1 |
101.0 |
22.5 |
29.5 |
66.7 |
763.5 |
123.0 |
886.5 |
1 Abbreviation of bio-climatic zones in Table x are:
T-tundra, FT-forest tundra, northern and sparse taiga, MT and
ST-middle and southern taiga respectively, TF-zone of temperate
forests, S-steppe, SD-semi-desert zone. Boundary of zones are given according
to the vegetation map edited by Isachenko (1990)
2 UFA and FL are unforested area and forest land, respectively
Forests are the major vegetation type in the taiga zone which is
presented by two major taiga sub-zones - middle taiga with an area
of 460 million ha and southern taiga - 130 million ha. Over 75
percent of the total Russian forested area is situated in these
two sub-zones. In European Russia, spruce, fir, and pine forests,
with considerable areas occupied by secondary birch and aspen forests,
dominate on the Al-Fe-humus and texture-differentiated soils. In
the Urals and West Siberia, considerable areas are covered by dark
coniferous forests of Siberian spruce, stone pine (Siberian cedar)
and fir, which have developed on burozems and metamorphic soils.
Vast territories of the taiga zone are composed of pine and larch
forest. Al-Fe-humus and metamorphic soils prevail in these forests.
The mountains of South Siberia and the Far East are occupied by
highly productive dark coniferous forests. Forests in the Altai
and the Sayan mountains are dominated by Siberian spruce, cedar,
pine, and Siberian fir. Spruce and fir forests, mostly composed
of Siberian spruce and fir, stretch up to the Far Eastern mountains.
These forests are developed on metamorphic soils to the east, up
to the Sikhote-Alin and Sakhalin. In the Amur Region and to the
south of the Amur River, the unique cedar-broadleaved forests are
formed by Korean cedar pine, Ajan spruce, different firs, and broad-leaved
tree species like oak, ash, lime-tree etc. which grow on metamorphic
and Al-Fe-humus soils. Upper forest belts of mountains from Zabaikal’je to
the east and north-east are often occupied by stone birch forests
that are replaced by Siberian dwarf-pine elfin woods of higher
altitudinal belts, which in turn are replaced by sub-alpine vegetation
of herbs and shrubs growing on thin, and as a rule, stony substrates.
Historically, both areas and distribution of Russian forests have
changed considerably. From 1700-1900, about 70 million ha were
deforested in European Russia; the forested area shrank from 19%
to 10% in this part of the country. Over the past 50 years, forested
areas in Russia have increased by about 80 million ha. This increase
is explained by more complete and accurate forest inventory data,
as well as by the boreal forests' great capacity for self-renewal,
significant fire suppression during this period, and substantial territories
of planted forests (the State Forest Account accounted for 18.8 million
ha of planted forests in 2003). At the same time, forest quality worsened
considerably, mainly in the regions of intensive logging, when the most
productive standing trees of valuable coniferous species were felled and
large areas of secondary forests are observed.
Russian forests are prone to numerous natural and human-induced
disturbances such as wild fires, insect outbreaks, diseases and
industrial pollution (see Section Disturbances).
Disturbance is one of the important drivers defining the condition
and dynamics of Russian forests. On average, 8-15 million ha of
forest land are substantially affected by different types of disturbances
annually. On-going climate change is dramatically increasing the
threat and damage of such disturbances as fire and insect outbreaks.
Political, social, and economic changes in Russia during the last
decades substantially impacted the governance of Russian forests
and accelerated a number of negative processes, in particular,
illegal logging. However, developments in recent years allow us
to conclude that there is evidence of positive development too
and some restoration of the Russian forest sector (see Section Forest Management).
Further reading:
Morozov G.F. 1970-1971. Selected Works. Vol.1, 1971, 30 pp. Vol.2,
1971, 30 pp. Lesnaya Promyshlennost', Moscow. [In Russian]
Forests of Russia. Encyclopedia. 1995. Under the general editorship
of A.I. Utkin, G.V. Lindenman, V.I. Nekrasov, and A.V.
Simolin. Bol'shaya
Rossiayskaya Ensyklopediya. Moscow, 446 pp. [In Russian]
Sukachev V.N. 1964. Forest Biocenology. Academy of Sciences of
the USSR, Moscow, 471 pp. [In Russian]
Zhukov A.B. (ed.). 1966-1970. Forests of the USSR. Volume 1, 2,
3, 4, 5. Academy of Sciences of the USSR, Moscow [in Russian]
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