1048
Figure 2. Schematic diagram showing the kinds of data
included in the modelling of supply and demand of
fuel-wood in semi-arid Sudan. Source: Olsson et.al.
(1985)
7.4 Combined supply/demand modelling
When quantifying e.g. vegetation amount by use of
remote sensing, the result is normally presented as
amount per area unit. When dealing with supply and
demand of resources, the aim is to translate the area
based measure into a per capita based measure, and
then compare, in one way or another, the supply with
the demand. I will briefly outline two different
attempts to model supply and demand, both carried out
in semi-arid parts of the Sudan, dealing with fuel-
wood (Olsson et.al. 1985 and Olsson 1985) and millet
production (Olsson 1985).
In the case of wood resources, the modelling was
based on Landsat MSS derived data on supply of woody
biomass (tons/ha) and estimated, by interviews,
annual consumption of wood, in Kordofan province of
the Sudan. The modelling compared the demand for each
village with the resources within a certain walking
distance, a schematic description of the different
kinds of data and analyses is presented in Figure 2.
As a result the walking distance needed to satisfy
the demand or the actual wood deficit was calculated
for each village. The methodology is readily appli
cable to studies on future development of the wood
situation, through simulation of different variables,
population increase, migration, afforestation, land
management etc.
In the case of millet production, the modelling was
based on population distribution and statistical
prediction of millet productivity. Spatial modelling
yielded detailed information on land availability
(Ha/capita). This was achieved by, following the rule
that a piece of land belongs to the nearest settle
ment, applying an algorithm delineating polygons
around every settlement (Thiessen polygons).
The number of hectars available per capita could
then be calculated and represented as a raster image.
The yield of millet was predicted from climtic data,
represented as a trend surface, and combined with the
land availability. The combination of productivity
estimates and land availability made it possible to
project the per capita production. When combined with
more accurate measurements of actual crop return,
based on remote sensing methodology, this approach
will be a powerful instrument for studies of spatial
distribution of food production.
7.5 Soil erosion modelling and prediction
Much research has been undertaken to establish
mathematical relationships between various landscape
features and rate of soil erosion. The most wellknown
example is perhaps the Universal Soil Loss Equation
(USLE) by Wishmeier & Smith (1960) , primarily
developed for North American conditions, but
subsequently adjusted for applications in other
areas. The traditional methodology for mapping of
erosion hazards is based on measurements in limited
catchments, from which approximations have then been
done. It is, however, today possible to apply a
mathematical erosion model in a GIS, in order to
carry out spatially full-covering mapping of poten
tial soil erosion. The most important factors
controlling erosion are topography, vegetation cover
and land use. All these factors can with high
accuracy and speed be treated using the combination
of remote sensing and GIS.
REFERENCES
Bartlett D.S., R.W.Johnson, M.A.Hardisky & V.Klemas
1986: Assessing impacts of off-nadir observation on
remote sensing of vegetation: use of the Suits
model. Int. J. Remote Sensing, vol. 7, pp 247-264.
Bauer M.E., J.E.Cipra, P.E.Anuta & J.B.Etheridge
1979: Identification and area estimation of
agricultural crops by computer classification of
Landsat MSS data. Remote Sensing of Environment
Vol:8 pp.72-92
Bush & Ulaby 1978: An evaluation of radar as a crop
classifier. Remote Sensing of Environment Vol: 7,
pp. 15-36
Cihlar J., R.J.Brown & B.Guindon, 1986: Microwave
remote sensing of agricultural crops in Canada.
International Journal of Remote Sensing, Vol 7, pp
195-212.
Cohen J. 1960: A coefficient of agreementof nominal
scales. Educational and Psychological Measurement
Vol:20, pp. 37-46. (in Rosenfield & Fitzpatrick-
Lins 1986)
Cohen J. 1968: Weighted kappa: Nominal scale
agreement with provision for scaled disagreement or
partial credit. Psychological Bulletin Vol: 70,
pp.213-220 (in Rosenfield & Fitzpatrick-Lins 1986)
Coiner J.C. 1980: Using Landsat to monitor changes in
vegetation cover induced by desertification
processes. Proc. 14th International Symposium on
Remote Sensing of Environment, pp.1341-1351.
Colwell R.N. 1956: Determining the prevalence of
certain cereal crop diseases by means of aerial
photography. Hilgardia Vol: 26 pp. 223-286. (in
Reeves 1975)
Crist E.P. & R.J.Kauth 1986:The tasseled cap de
mystified. Photogrammetric Engineering & Remote
Sensing Vol:52, pp 81-86.
Curran P.J, 1980: Multispectral remote sensing of
vegetation amount. Progress in Physical Geography,
Vol: 4, No: 3, pp. 315-341.
Curran P.J,
Longman, I
Duggin M.J.
Evaluation
Applied Op
Ewalt D. 19
study Vol.
Report 15
Townshend
Graetz R.D.,
1982: Th
resource
applicatic
Australian
Symposium
Lands, Cai
Guignard J.
and operat
Journal Vc
Haralick R.M
and spatia
Sensing of
Hay A.M. 19
accuracy.
Sensing Vc
Hellden U.
digital da
an enviro
University
& Notiser-
Hellden U.,
remotely
the Sudan.
Rome 2-6 D
Hoffer R.M
consider at
techniques
Swain & Da
Holben B.N.
assessment
Photogramm
46 pp. 651
Hord R.M.
criteria.
Sensing Vo
Hugli H. &
reflectanc
Engineerin
Hutchinson
Landsat a
cation im
Remote Sen
Justice C.O.
1985: Ana
tion Using
Journal of
Kauth R.J.
graphic
developmen
Landsat.
Remote Sen
Ch. 1103-1
Kettig R.L.
multispect