Forestry possibilities in Ethiopia
By E.H.F. SWAIN, FAO TECHNICAL ASSISTANCE
ADVISER IN FORESTRY
AFTER a six month's sojourn in Ethiopia
one does not speak with authority on forestry for a land as large
as France and Germany combined. One can do little more than present
an impressionistic sketch of information absorbed and of deductions
tentatively reached, and pay tribute to the two preceding pioneers
and reporters of forest explorations in this little known country,
namely W.E.M. Logan, Assistant Conservator of Forests for the
Gold Coast, whilst on war service in Ethiopia, and Glen Russ
of the U.S.A. Technical Mission of 1944-1946.
The general background
Forest conditions are largely shaped by
the interaction of men and trees. The elements of the Ethiopian
interaction appear to have been as follows.
1. A people, contented and courteous, who
have dwelt apart from world influences in highlands of rarefied
air surrounded by lowland deserts.
2. The preoccupation of this free and independent
people with agricultural and pastoral production, for simple
subsistence from red and black soils on which famine and malnutrition
are unknown, and which now support about 15,000,000 people.
3. Free selection of land from the outset
of colonization, without benefit of surveys or title-deeds; dispossession
and changed possession as the outcome of wars; Imperial grants
of entailed freehold (gultrist) and of unentailed free-hold
(rists); Imperial leaseholds and tenancies.
4. The tradition that useable trees are
"royal trees" belonging to Emperor and Government but
not yet registered in written laws and still uncertain of application
to rist lands.
5. The settlement practice of leaving "royal
trees" standing, but of clearing the land around them and
burning the trash so that the "royal trees" also succumb.
6. Forest denudation, spreading from the
drier north into the moister south, leaving soils stripped of
forests, from which the humus has vanished and the surface soils
have been washed away.
7. The survival of virgin forests among
the hills of the south and south-west, where carnivora, malaria,
wars, topography and the general absence of roads have reduced
population pressures upon the land, and where the forests are
commercially quite inaccessible.
8. The annual clearing by fires on the
southern forest fronts, to mark the continuing advance of an
agricultural people in pursuit of new farms for old.
9. Traditional satisfaction with local
production for local "wayside markets."
10. The relative unimportance, to this
indigenous economy, of roads and highways.
11. Historic independence of the world's
economy, not significantly affected by the narrow-gauge railway
from a political capital across an unproductive desert to a foreign-held
port. Trade mainly consists of an exchange of coffee and hides
for cotton and paper (which Ethiopia could itself produce), and
motor cars and modern goods largely for the governing group and
the small foreign population.
12. The dawning of a new era of stationary
administration in a permanent capital, superseding a history
of shift from center to center in search of fresh stands of trees
for fire-wood and building timber for the needs of the Imperial
community. This new era was made possible in 1906 by the introduction
and planting of Eucalyptus globulus on the Entotto hills,
whence the stands of native juniper (often called cedar) had
been quickly stripped.
13. A still unfinished unification of Ethiopia
pending:
(i) the development of modern roads through
difficult country to all parts of Ethiopia;
(ii) the maturing of administrative organization
and the perfection of laws and systems in a new center of Government;
and the extension of like organization to the provinces.
14. A post-war Ethiopian renaissance, under
the personal inspiration of His Imperial Majesty, Haile Selassie,
Emperor of Ethiopia, who has been quick to perceive that the
pressures of a multiplying world population oblige Ethiopia to
make adequate dispositions for the future.
15. Lingering doubts of modern ideas of
economics and of the political systems of the outer world.
This, then, is the background to forestry
in Ethiopia. In the face of many difficulties, in the teeth of
ancient rights and customs, in a multilingual medium which delays
any form of action, the Ministry of Agriculture is attempting,
with FAO assistance, to shape Ethiopia's first forest policy
out of these diverse elements.
Before, however, one can write the recipe
for a forest policy, one has first to study the ingredients,
Climates, Forests and Economic Routes.
Ethiopia (Map)
Climates of Ethiopia
Ethiopia lies near the Equator, at 3°
to 18° Lat. N., resulting in warm temperatures with narrow
seasonal differences. The country, however, drops to 100 meters
below the level of the Red Sea and then lifts sharply to 2,250
meters, to provide a rugged base for mountain peaks some 4,000
meters above the sea. From these mountains the rainfall then
creates the torrents which have dissected the rugged base itself
by riverine gulfs 500 to 1,300 meters deep.
On this terrain we find a stratification
of seasonally narrow climates, modified by regional variations
in rainfall resulting, according to the elevation, in everything
from torrid deserts up to winter-frosted peaks on which hailstorms
take the place of snow.
In none of this series do temperatures
of themselves inhibit the development of forests composed of
appropriate species. The limiting factor of a country which helps
to fill the Nile with water is drought.
The mean annual rainfalls of Ethiopia range
from 25 to 2,500 mm., yet what determines the distribution of
vegetation is not the isohyet, but the duration of the annual
dry season, which may be measured by simply counting the number
of months in the year in which the monthly rainfall average is
less than 60 mm. or 2 inches.
Thus, Adamitullo and Shashamana, in the
Ethiopian Rift, each registers around 600 mm. mean annual rainfall,
but vegetation at Adamitullo has to survive six dry months in
the year, whilst that of Shashamana must endure seven or eight.
Gambela and Bure, in the rainy south-west,
each record a mean annual rainfall of 1,270 mm., but Gambela
has five dry months, and Bure only three. The flora of Bure,
if called upon to outlast five dry months instead of three, would
be much reduced in composition and yield. Gambela and Bure are
in different rainfall regimes as well as in different temperature
regimes, and each has its own flora frequency. Throughout the
country there are many parallel examples of this and it is in
fact the length of the dry season which decides the forest distribution.
Unfortunately, there are at present only 10 meteorological stations
in Ethiopia and these are the sole source of data on climatic
conditions. Knowledge of the vegetation and the altitudes must
be drawn upon to fill in the details, as for example by considering
the distribution of coffee growing.
Coffee is a plant decreed by nature to
be a denizen of lands without frost or drought. Of the three
commercial species in the world, C. robusta and C.
liberica cannot survive even in the rainiest parts of Ethiopia.
C. arabica has the most endurance of the three and special
strains have been developed for Ethiopia. These strains are only
successful (without irrigation) where the number of dry months
does not exceed three, and is more than one. Thus, we have the
Ethiopian coffee belt climatically defined as below the frost-line
of about 2,240 meters altitude, in a rainfall regime of 2-3 dry
months.
The Landolphia rubber liane and the broad-leaved
trees of East Africa, (but not of drought-free Central Africa)
are within this coffee-rainfall regime. But Juniperus procera
is suited instead to higher, colder and drier elevations,
where it puts on an inch of diameter growth in ten years. Between
these two extremes, or in the shelters of the lesser heights,
grows Podocarpus gracillior.
So, despite meagre meteorological data,
we can still construct a climatic pattern for Ethiopia-Eritrea,
as the basis for consideration of the area's forest problems.
This pattern is shown in the accompanying table.
Between coldest and hottest month, the
modal range is 57 degrees Centigrade. In the dry lowlands, it
widens to 8-10 degrees - except in the south-western desert of
Ogaden, where the higher winter temperatures narrow it. It reaches
its maximum range on the Eritrean Highlands, where summer drought
permits the fullest play of sun heat. Elsewhere, the rule is
that rains and cloudiness depress the summer thermometer and
leave it to the drier spring to provide the hottest month of
the year, as the "Ethiopian Summer."
Whilst seasonal differences of temperature
are abnormally small differences of temperature between day and
night are abnormally great. Judged by day temperatures only,
the wet-cloudy summers are colder than the dry winters, and Ethiopians
regard the calendar summer as "winter time." But the
night temperatures of the calendar winter are low enough to give
that season the mean temperature of the coldest month, both on
highlands and lowlands.
Ethiopians do not appreciate adherence
to the calendar seasons in preference to their own sense of heat
and cold, and it must be accepted that exotic trees appear to
incline to the Ethiopian view. These are some of the difficulties
of understanding the climatic whys and wherefores of the Equatorial
Highlands.
Forest types
If you place your left hand upon the table
with the fingers closed and the thumb extended, you have a rough
outline of Ethiopia set upon its deserts, and sloping from right
to left. The fingers are the northern highlands, the knuckles
its peaks, and the interstices the river-cut gulfs. The back
of the hand is the southern belt of lowest drought period and
of highest productivity. The thumb continues as a bridge to the
desert borders of the seaport of Berbera in British Somaliland.
Obviously, the forest climates of Ethiopia
are those of this highland hand, with Regime No. 4 of 5 dry months
along the fingers and Regime No. 5 of 2-4 dry months on the back.
The forests of Regime No. 4 have been reduced to remnants by
a thousand years of southward march from Axum. The forests of
Regime No. 5 are experiencing the same reduction in the south-east.
In the remote and inaccessibile south-west, they linger intact
and as yet unused.
Nevertheless, the forests which survive
the hand of man in Ethiopia to-day measure approximately 500,000
hectares. That is three times the extent of the high forest of
adjoining Kenya, whence exports of manufactured timber of identical
East African trees find their way to overseas markets over 600
miles (965 km.) of railway - whilst Ethiopia can export none,
for want of access routes.
A number of attempts have been made to
classify tropical woody vegetation types. In 1938, T. Burt Davy,
mainly on the basis of Indian data, defined six principal types,
as follows:
1. High Montane Conifer Forest
2. Upper Montane Rain Forest
3. Lower Montane Evergreen Rain Forest
4. Moist Deciduous Forest
5. Lowland Evergreen Forest
6. Semi-Evergreen Forest
In spite of their 1,300 to 6,300 mm. of
mean annual rainfall and their general title of "rain forest,"
the essential limitation of these six tropical woody vegetation
types is their annual drought period.
There is definite correspondence between
Davy's High Montane Conifer Forest type (Champion's Dry Coniferous
Forest of India) and the type of Ethiopian coniferous forest
of Regime 4 (c), with its five dry months and its 700-1,300 mm.
of mean annual rainfall. The Ethiopian indicator species are
Juniperus procera, mixed with Hagenia abyssinica,
Olea chrysophylla, Rhus, Ilex, Allophylus,
Bersama and Schefflera. The same Juniperus type,
with Olea and Widdringtonia, frequents the 2,000-3,000
meters altitudes of Kenya in an equivalent climatic regime. It
is found again towards sea-level in the Union of South Africa
far to the south, but drought periods and temperatures again
indicate the reasons for its occurrence there, with latitude
compensating for altitude.
Regimes 4 (a) and 4 (b) of Ethiopia have
similar temperatures to those of Davy's Lower Montane Evergreen
rainforest, but their diminished rainfalls and doubled drought
period exclude his wood vegetation type. Regime 5 (a), however,
admits it, but with reduced mean annual rainfall.
CLIMATIC REGIMES IN ETHIOPIA
|
Area |
Altitude (m.) |
Mean Temperatures Cold Months °C |
Mean Temperatures Hot Months °C |
Mean Annual Rainfall (mm.) |
Number of Dry Months |
|
1. Regimes of 11 - 12 dry months |
|
(a) Ogaden Desert (S. E. Ethiopia) |
300-1000 |
24-29 |
29-34 |
50-125 |
12 |
|
(b) North-western Eritrean Uplands |
300-1670 |
23-28 |
32-36 |
50-200 |
12 |
|
(c) Eritrean and Danakil Coastal Deserts |
0-1000 |
21-26 |
31-36 |
25-200 |
11 |
|
(d) Awash Desert |
1-1000 |
20-24 |
29-33 |
150-250 |
11 |
|
2. Regimes of 8 - 10 dry months |
|
(a) North-west (Sudan) Slopes of Ethiopia |
500-1000 |
23-26 |
30-33 |
400-650 |
8 |
|
(b) Low Somali Slopes (S. E. Ethiopia) |
1000-1670 |
19-23 |
24-28 |
250-500 |
8 |
|
(c) Eritrean Highlands |
1000-1670 |
18-22 |
28-33 |
350-500 |
9-10 |
|
(d) Eritrean Highlands |
1670-2240 |
16-18 |
21-27 |
500-750 |
8-9 |
|
(e) Eritrean Highlands |
2240-3000 |
8-16 |
14-20 |
450-550 |
10 |
|
3. Regimes of 6 - 7 dry months |
|
(a) West (Sudan) Slopes of Ethiopia |
500-1000 |
23-27 |
30-34 |
800-1000 |
6-7 |
|
(b) Rift and the Harar Escarpment |
1000-1670 |
17-22 |
24-29 |
500-800 |
5-7 |
|
(c) Low Somali Slopes of S. E. Ethiopia |
1000-1670 |
17-20 |
24-27 |
500-600 |
6-7 |
|
(d) North-east Escarpment of Ethiopia |
more than 2240 |
11-13 |
16-18 |
1000-1500 |
6 |
|
4. Regimes of 5 dry months |
|
(a) Harar Tableland |
1670-2240 |
16-19 |
19-22 |
750-1000 |
5 |
|
(b) North-west Highlands of Ethiopia |
1670-2240 |
14-17 |
20-22 |
1200-1450 |
5 |
|
(c) North-east Highlands of Ethiopia |
2240-2760 |
13-15 |
18-19 |
700-1300 |
5 |
|
(d) South-west (Sudan) Slopes of Ethiopia |
500-1000 |
22-26 |
28-31 |
850-1300 |
5 |
|
5. Regimes of 2 - 4 dry months |
|
(a) Galla Highlands |
1670-2240 |
17-19 |
22-26 |
1300-2000 |
2-4 |
|
(b) Arussi-Bale Highlands |
1670-2240 |
- |
- |
1200-1750 |
2-3 |
|
(c) Arussi-Bale Highlands |
more than 2240 |
- |
- |
1200-1750 |
2-3 |
|
(d) Eritrean Escarpment |
500-1000 |
18-20 |
20-31 |
700-900 |
3 |
|
(e-f) Eritrean Escarpment |
1000-2240 |
- |
- |
- |
- |
|
(g) Eritrean Escarpment |
2240 |
13-14 |
20-21 |
1000-1200 |
3 |
A drought prolongation and diminished rainfall
changes Davy's Lower Montane Evergreen Forest into his Moist
Deciduous forest, as represented by the Teak and Terminalia
Forest of India and the Padauk of the Andamans. That section
of the Ethiopian Regime's No. 5 (a) of highest rainfalls and
least drought period, however, barely admits this type - excluding
the deciduous trees and converting the type to his Lowland Evergreen
Forest, as recorded for India and Ceylon from sea-level to 900
meters.
Davy's Semi-Evergreen Forest is only a
differentiation of his Lowland Evergreen type, registering the
period of inadequate soil moisture. It exists as an ecotone between
closed forest and parkland, or as a connecting link between moist
deciduous and dry tropical forest. Regime 4 (d) of Ethiopia approximates
to Davy's Semi-Evergreen forest, but it is hotter and drier,
with corresponding effect upon the indigenous woody vegetation.
Davy's High Montane Rainforest approximates
to the Temperate Rainforest of Shantz and Marbutt, who, however,
group Juniperus procera and Podocarpus gracilior forests
together. Yet both are Drought Period forests. The Tropical Rainforest
of Shantz and Marbutt, recorded for the Ivory Coast and the Cameroons,
has no place in Ethiopia, because Ethiopia has no such moist
climatic regime.
W.E.M. Logan applies the name of Tropical
Upper Montane Rainforest to both the Ethiopian Podocarpus
forest and to the Ethiopian broad-leaved forests of regime 5
(a) combined. He uses the High Montane Conifer Forest type of
Davy for the Juniperus forests, but precedes it with the
adjective "tropical," though the type extends from
the Sudan edge of Northern Eritrea southwards to Cape Province.
Glen Russ dismisses all the extant rainforest
classifications as incompatible with the forest types of Ethiopia
and adopts, instead, the differentiations:
1. Coniferous Mixed Forest
2. The Broad-Leaved Forests of the South-west and West
3 The Gallery Forests
This is a simple and direct classification,
but oversimplified.
All these classifications lack essential
correlation with their climatic regimes, of which their forest
types are true vegetational expressions. Nor would 1, at this
stage, wish to attempt this fundamental but complex task for
a territory where climates are confused by a complicated topography.
It does not take long to perceive, however,
that Juniperus procera can tolerate five dry months per
annum on the thin-soiled, frosted backbones of Ethiopia, and
that this Temperate Mixed Juniper Forest deserves distinction
from the Temperate Mixed Podocarpus Forest which Glen
Russ groups with it.
Podocarpus gracilior cannot ascend the hard heights of the dry hills
nor reach the desert edges, nor can it spread as far north or
south as Juniperus. Its growth-rate is almost as slow,
but its drought-resistance is lower. It seeks a milder habitat
and the companionship of less hardy broad-leaved species. It
finds its place in lower, sheltered vales where it is joined
by the more venturesome broad-leaved trees of the narrow drought
period regimes, such as Ekebergia ruepellianum, Celtis
kraussianum, Olea hochstetteri, Syderoxylon acantha
and Apodytes. Though the Podocarpus vales interlace
with the Juniperus hill-crests, and though both species
mingle at the margin (but with Podocarpus always sheltering
under the Juniperus) their characteristics, and habitats
and types are different.
The Temperate Mixed Podocarpus Forest
is really the link between the Temperate Mixed Juniperus
Forest and the Sub-Tropical Broad-leaved Forests of the 2-4 dry
months climatic regime - a type which Logan styles the Pouteria-Albizzia
Association of his Tropical Upper Montane Rainforest, and
which Russ disposes of as the Broad-leaved Forests of the South-west
and West, of the Ethiopian Highlands.
Between them, they record for these broad-leaved
forests the following timber trees with no Central African species
among them:
Pouteria (Sersalina) ferruginea
Albizzia schimperiana
Sapium ellipticum
Allophylus abyssinica
Gallineria coffeoides
Schefflera abyssinica
Dracaena steudneri
Polyscias ferruginea
Milletia ferruginea
Teclea nobilis
Maesa lanceolata
Pygeum africanum
Ficus sp. (at their optimum)
Cordia abyssinica
Croton microstachya
Mitragyna sp.
Erythrina sp.
It is the forest types of the forest climates
cited above, which give to Ethiopia its now man-reduced forest
area of 500,000 hectares; an area which yet might be doubled
by reforestation.
These, however, do not exhaust the forest
potential of Ethiopia. Climatic Regime 3, which registers 6-7
dry months per year, is the habitat of Logan's Tropical Savannah
Woodland, Russ's High Grass Savannah, or Shantz and Marbutt's
Tropical Dry Forest. Annual grazing fires have degraded this
dry forest type, reduced its constituent species to the most
fire-hardy and widened their spacing to that of an orchard. The
surviving species are of such genera as Combretum, Terminalia,
Schrebera, Zizyphus, Syzgium, Lonchocarpus,
Iannea, Faurea, Stereospermum, Gardenia,
Cussonia, Hymenodicton, Hauswolfea, Gymnosporea,
Acacia, Vitex Ehretia, Bauhinia, Protea,
Grewia and Dodonea. The last seven genera are represented
in Australia in an equivalent climatic regime.
Given fire-protection and a sand-mulch,
the Australian Callitris glauca, cousin of the East African
Widdringtonia, could make a forest stand here. Several
Australian Eucalyptus could also distinguish themselves; thornless
Australian Acacias would find themselves at home - more
so than Acacia senegal, the producer of gum arabic which
flourishes in the 6-7 dry months zone of Eastern Sudan, with
650 mm. mean annual rainfall on black, cracking clays, or 450
mm. on sand (and provides the Sudan with 20,000 tons of exports
per annum).
The latter species, however, demands a
higher summer heat than most of the Ethiopian 6-7 dry months
regime affords. It reappears therefore on the coastal and lakeside
lowlands of Kenya where it can keep warm enough to make gum arabic
- yet with enough dry months to exude its gum from its cracking
bark.
Russ describes this dry forest type as
the most widespread of Ethiopia, covering half the country. It
develops below the high forests, and descends the slopes, through
lengthening drought periods, until it has to give place to Russ's
Desert Acacia Savannah, Logan's Tropical Thornland, or Shantz
and Marbutt's Thorn-Forest - where the dry months range from
eight to eleven per annum, and the forest potential of Ethiopia
comes to its end in perennial drought.
Exotics
Thus we get a glimpse of Ethiopia's forest
situation. The behavior of exotics throws more light on the subject.
Towards the end of the last century Menelik
II brought his court to that place where his empress thought
to build the "City of the New Flower" in the shadows
of the broad, high hills of Entotto. Those hills were thick Juniperus-Podocarpus
forests and gave promise of wood provision for all time to
those whom forest denudation had driven out of the place from
which they had just come.
Menelik II thought to make assurance doubly
sure by re-declaring, as oral law, the ancient tradition of imperial
ownership of full grown trees. He failed to realize that this
could be insured only by safeguarding the younger trees to maturity.
Thus, he missed becoming the founder of Ethiopian forest policy.
He permitted the continuance of clearing younger trees for cultivation,
and they in turn provided the fuel for the fires which brought
both Imperial trees and Imperial law to nothing.
The Entotto hills became completely stripped.
It appeared that the gardeners of this "City of the New
Flower" would be expelled once more from their would-be
Eden to seek wood in the underlands of Galla.
At this juncture there arrived M. Mondon-Vidaillet,
a French forester, with seeds of Australian Eucalypts. One of
them was a tough tree from the hard Australian hills, accommodating
enough to take both winter and summer rainfalls in its stride,
as well as snow. It grew prodigiously. It was planted at 20,000
per hectare, and thinned for its produce in the fourth, seventh,
fifteenth and twenty-fifth years. The 800 trees left per hectare
had a standing volume of 570 cubic meters in the 26th year and
1080 cubic meters in the 40th.
The thinnings gave staves for fences, slim
sticks for wattle and daub toukouls, and finally, tall
poles for the scaffolding of the Imperial masonry. There was
also firewood in plenty, even to the bales of foliage lumbered
to the toukouls for the cooking of the ingera pancakes
of the people.
Anyone who wanted to make good his future
planted a plot of this Bahaar Zarf, this "Strange
Tree from across the Sea." Now, forestry is the chief industry
of the environs of the capital city of Addis Ababa with its 300,000
population. On any market day you will see the forest owners
converging on the city, and on their backs and heads and overwhelming
their tiny donkeys the produce of their investment. They provide
90 percent of the market traffic. All this is owed to one species
of tree.
Now, there are others on trial. Grevillea
robusta flaunts its sprays of old gold in the dry Ethiopian
autumn, similar to the dry Australian springtime. The Australian
blackwood gum grows with the Australian blue Gum; the Australian
black wattle of the tanneries flourishes as do the Casuarinae.
Mexican, Californian and Mediterranean Cypresses thrive, although
the sudden drought period mortally splits the bark of weaklings.
A Norfolk Island Pine grows strongly, and you may see the Californian
Pinus radiata top-blighted by the north-east winter heat
on the her of hills, yet thriving in sheltered valleys.
The significant thing about these exotic
successes ix that they all came from drought period habitats,
and have had to survive the primitive techniques of sowing in
February at the scant commencement of the rains and open-root
planting six months later in the deluges that herald the long
drought from October back to February again.
With a more scientific approach and techniques,
therefore, Ethiopia might well come to be able to grow a vast
new forest estate.
Conclusion
It does indeed seem from a cursory survey
that Ethiopian forests might provide means of development of
the country's economic life. An obvious first step forward is
the diversion of trained youth into the creation of a forest
service and forest industries. There is still, however, a lion
in the path of such a forest policy, and, indeed, in the path
of the entire Ethiopian Renaissance. No country was ever developed
except along with economic transport routes.
Neighboring countries have had to do it,
and Ethiopia can do it - and more profitably, because no neighbor
x ever had such a continuous belt of potential productivity through
which to project its main road to development.