UoG Dept of GeES 1 UNIVERSITY OF GONDAR COLLEGE OF SOCIAL SCIENCES & HUMANITIES Department of Geography & Environmental Studies Agro ecology and farming system (GeES3103) CHAPTER ONE INTRODUCTION 1.1, The Concept of Ecology and Agro ecology and Farming System A, Ecology Origin of the word…”ecology” that is, it is a Greek origin: OIKOS = household, LOGOS = study. Therefore, Study of the “house/environment” in which we live. Ecology is study of interactions between non-living components in the environment such as light , water, wind, nutrients in soil, heat, solar radiation, atmosphere, etc. and Living organism, such as Plants, Animals, microorganisms in soil, etc. It views each locale/ environment as an integrated whole of interdependent parts that function as a unit. The interdependent parts are Nonliving such as dead organic matter, nutrients in the soil and water; Producers such as green plants; Consumers such as herbivores and carnivores; Decomposers such as fungi and bacteria. Then, ecology is an integrated and dynamic study of the environment; the study of living organisms in the natural environment. How they interact with one another How they interact with their nonliving environment. B, Agro ecology A wider understanding of the agricultural context requires the study between agriculture, the global environment and social systems given that agricultural development results from the complex interaction of a multitude of factors. It is through this deeper understanding of the ecology of agricultural systems that doors will open to new management options more in tune with the objectives of a truly sustainable agriculture. Different scholars’ definition Gliessman 2000 defined: “The application of ecological concepts and principles to the design and management of sustainable farming systems. Ecological concepts and principles: understanding science Design and management: practice (technology)
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UoG Dept of GeES
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UNIVERSITY OF GONDAR COLLEGE OF SOCIAL SCIENCES & HUMANITIES
Department of Geography & Environmental Studies Agro ecology and farming system (GeES3103)
CHAPTER ONE
INTRODUCTION
1.1, The Concept of Ecology and Agro ecology and Farming System
A, Ecology
Origin of the word…”ecology” that is, it is a Greek origin: OIKOS = household, LOGOS = study. Therefore,
Study of the “house/environment” in which we live.
Ecology is study of interactions between non-living components in the environment such as light , water, wind,
nutrients in soil, heat, solar radiation, atmosphere, etc. and Living organism, such as Plants, Animals,
microorganisms in soil, etc. It views each locale/ environment as an integrated whole of interdependent parts that
function as a unit. The interdependent parts are Nonliving such as dead organic matter, nutrients in the soil and
water; Producers such as green plants; Consumers such as herbivores and carnivores; Decomposers such as fungi and
bacteria.
Then, ecology is an integrated and dynamic study of the environment; the study of living organisms in the
natural environment. How they interact with one another How they interact with their nonliving
environment.
B, Agro ecology
A wider understanding of the agricultural context requires the study between agriculture, the global environment and
social systems given that agricultural development results from the complex interaction of a multitude of factors. It is
through this deeper understanding of the ecology of agricultural systems that doors will open to new management
options more in tune with the objectives of a truly sustainable agriculture.
Different scholars’ definition
Gliessman 2000 defined: “The application of ecological concepts and principles to the design and management
of sustainable farming systems.
Ecological concepts and principles: understanding science
Design and management: practice (technology)
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Sustainable: goal and motivation (What is sustainability? How does sustainability vary? What makes a
farming system sustainable? Is sustainability always attainable?)
Farming systems: techniques
B. Boeken defined that: The application of ecological concepts and principles to farming systems
Ecological concepts and principles: ecological processes associated with farming
Farming systems: All agro-systems (Conventional, traditional and Alternative agriculture)
The science of agro ecology, is defined as the application of ecological concepts and principles to the design and
management of sustainable agro ecosystems, provides a framework to assess the complexity of agro ecosystems.
Agro ecology is the study of the interactions between living organisms and their environment in agricultural systems.
The idea of agro ecology is to go beyond the use of alternative practices and to develop agro ecosystems with the
minimal dependence on high agrochemical and energy inputs, emphasizing complex agricultural systems in which
ecological interactions and synergisms between biological components provide the mechanisms for the systems to
sponsor their own soil fertility, productivity and crop protection.
Agro ecology has emerged as the discipline that provides the basic ecological principles for how to study, design and
manage agro ecosystems that are both productive and natural resource conserving, and that are also culturally
sensitive, socially just and economically viable. Agro ecology goes beyond a one-dimensional view of agro
ecosystems —their genetics, agronomy, and so on to embrace an understanding of ecological and social levels of co
evolution, structure and function. Instead of focusing on one particular component of the agro ecosystem, agro
ecology emphasizes the interrelatedness of all agro ecosystem components and the complex dynamics of ecological
processes.
Agro-ecology has been defined as a science, as a set of practices, and even as a social and political movement.
1. Agro-ecology as a science in its simplest form is seen as the “application of ecological science to the study,
design and management of sustainable agro-eco systems”. This can apply not just at the farm-level, but also
across the global network of food production, distribution and consumption, including food production
systems, processing and marketing, the role of the consumer, and the policy level. As such, it uses
knowledge from a range of disciplines, including agricultural and ecological science, and traditional
knowledge systems. It questions conventional approaches which are centered on the use of science to
promote economic growth.
2. Agro-ecology as practice -seeks ways to enhance farming systems by mimicking natural processes, using
biological interactions and synergies to support production.
3. Agro-ecology as a social and political movement is about how individuals, communities and societies
contribute to building sustainable, fair food models through what they buy, but also in the ways in which
they shop and organize food distribution. Agro-ecological movements seek to influence national and
international policies through grassroots cooperation, participation and action to create more sustainable
management systems for food and seeds
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Agro ecology is a discipline that defines, classifies and studies agricultural systems from an ecological and socio-
economic perspective, and applies ecological concepts and principles to the design and management of sustainable
agro ecosystems. Agro ecology is first and foremost a response to the negative ecological, social and economic
impacts of industrial agriculture.
The ecological perspective, focusing on how natural resources - soil and water are used and managed for
sustainable agricultural production;
The economic perspective, focusing on the marketing of agricultural products through competitive value
chains which link farmers to the consumer; and
The social perspective, focusing on how stakeholders interact, who controls change in agricultural practices,
and how to ensure that the benefits of innovation are enjoyed by all sectors of society including the poor and
previously disadvantaged
Hot topics in agro ecology
§ Pesticide effects on biodiversity
§ Mixtures of pesticides and effects on organisms
§ Endocrine disrupting effects of pesticides and industrial chemicals
§ Genetic engineering and “genetic pollution” in environment
§ Soil food web- function of diversity
§ Nutrient cycles
§ Industrial waste--toxic waste and application to land of heavy metals and dioxin in fertilizers
C, Farming system
Farming as a system
A farm = A system
Inputs into the system
Processes taking place in it
Outputs from the system
e.g. profits can be reused back in the system
1. Physical inputs
Climate
Amount and season of rain
Summer and winter temperature
Growing season
Relief
Soils and drainage
2. Human and economic inputs
Labor
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Rent
Transport costs
Machinery
Fertilizers and pesticides
Government control
Seeds – livestock
Farm buildings
Energy (electricity)
Farming systems vary within and between countries because of different:
Physical conditions
Human conditions
Economic conditions e.g. rice farming in India is quite different from the system of mixed farming in
England
Farmer as a decision maker
has to decide which crops to grow or which animals to rear => decision based on
physical factors
human factor
economic factors
chooses the type of farming most suitable to the conditions
using the most efficient method to gain maximum profit
A system is a set of inter-related, interacting and interdependent elements acting together for a common purpose and
capable of reacting as a whole to external stimuli. It is unaffected by its own output and it has external boundaries
based on all significant feed backs.
Farms are systems because several activities are closely related to each other by the common use of the farm labour,
land and capital, by risk distribution and by the joint use of the farmer’s management capacity. The analysis of farms
is quite important to the subject of development.
Farming systems refers to an ordered combination of crops grown, livestock produced, husbandry methods and
cultural practices followed. What do we mean by cropping systems? And farming systems?
1. Cropping systems refer to
key information about type of crops being grown and for what number of crops in a season – cropping
intensity
intercropping is similar but the crops are grown in lines
mixed cropping – different crops in the same field – planted more or less randomly
mono cropping
2. Farming systems is more holistic:
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all farm enterprises
describes how agriculture fits the farmers’ livelihood strategy
influence on environment, socio-economic factors, rural economy and politics
Characteristics of farms:
1. Goal orientation
A farm is taken to be an organized decision-making unit in which crop and/or livestock production is carried out with
the purpose of satisfying the farmers goals on large scale market production and profits are the main objectives
whereas for the small-holder farmer who farm most of the tropics the farm is a multi-objective system to provide
food for the household, raw materials for building huts, accumulation of capital in form of animals or plantations and
accumulation of wealth
2.Boundaries
The farm as a system has a boundary that separates the system from the environment. The system embraces all
workers and resources (elements of the system) which are under the management of the farmer
1.2, Ecosystem and agro ecosystem
A, Eco system = the Community + Abiotic environment, interacting
Levels of Organization; - a hierarchy of organization in the environment:
Biosphere; Surface of the earth and it composed of many ecosystems
Ecosystems: communities of organisms interacting with each other and with their physical environment
i.e. Community + Abiotic environment, interacting
Biodiversity: the variety of organisms living in an ecosystem. The total number of different species in an
ecosystem and their relative abundance
Organism – simplest level of organization (e.g., fish)
Population – one species live in one place at one time (e.g. many fish)
Community – All populations (diff. species) that live in a particular area (e.g. many fish + other
organisms). All the populations of the different species living and inter-acting in the same ecosystem
Habitat – physical location of community. The characteristics of the type of environment where an
organism normally lives (e.g. a stoney stream, deciduous temperate woodland)
B, Agro ecosystem
Agro ecosystems are communities of plants and animals interacting with their physical and chemical
environments that have been modified by people to produce food, fiber, fuel and other products for human
consumption and processing. The main focus of sustainable agro ecosystems lies on the reduction or elimination of
agrochemical inputs through changes in management to assure adequate plant nutrition and plant protection through
organic nutrient sources and integrated pest management, respectively. Agro ecology is the holistic study of agro
ecosystems, including all environmental and human elements. It focuses on the form, dynamics and functions of their
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interrelationships and the processes in which they are involved. An area used for agricultural production, e.g. a field
is seen as a complex system in which ecological processes found under natural conditions also occur, e.g. nutrient
cycling, predator/prey interactions, competition, symbiosis and successional changes. Implicit in agro ecological
research is the idea that, by understanding these ecological relationships and processes, agro ecosystems can be
manipulated to improve production and to produce more sustainably, with fewer negative environmental or social
impacts and fewer external inputs
1.3, Fundamental principles of agro ecology
Enhance recycling of biomass and optimizing nutrient availability and balancing nutrient flow.
Securing favorable soil conditions for plant growth, particularly by managing organic matter and enhancing
soil biotic activity.
Minimizing losses due to flows of solar radiation, air and water by way of microclimate management,
water harvesting and soil management through increased soil cover.
Species and genetic diversification of the agro ecosystem in time and space.
Enhance beneficial biological interactions and synergisms among agro biodiversity components thus
resulting in the promotion of key ecological processes and services.
promote agro-biodiversity, as the point of entry for the re-design of systems ensuring the autonomy of
farmers and Food Sovereignty;
foster and equip the multi-criteria steering of agro ecosystems in a perspective of long term transition,
including arbitrations between short time and long time and attaching significance to resilience and
adaptability properties;
promote the spatio temporal variability (diversity and complementarities) of resources, i.e. take advantage
of local resources and characteristics and work with diversity and variety rather than seek to overcome it;
Stimulate the exploration of situations far removed from optima already known, e.g. “extreme” systems at
very low levels of inputs and/or organic in livestock as well as in vegetable production
Promote the construction of arrangements for participatory research that allow the development of
“finalized” research while guaranteeing the scientificity of approaches. The design of sustainable systems
indeed is complex and implies the acknowledgment of interdependence of actors, of their ambiguities, as
well as of the uncertainty of socio-economic impacts of technological innovations;
create knowledge and collective capacity of adaptation through networks including producers, citizens-
consumers, researchers and technical advisers of public authorities, which promote deliberative forums,
public debate and knowledge dissemination;
promote possibilities of choices of autonomy compared with global markets by the creation of a public
goods-friendly environment and the development of socio-economic practices and models which
strengthen democratic governance of food systems, notably via systems managed by producers and
citizens-consumers and via systems (re)territorialized highly labor intensive;
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Promote the diversity of knowledge to be taken into account: local or traditional knowledge and practices,
ordinary knowledge in the construction of problems and the construction of publics concerned by these
problems, than in the search of solutions.
Specific interpretations are given as follows
1. Use Renewable Resources Use renewable sources of energy instead of non-renewable sources.
Use biological nitrogen fixation.
Use naturally-occurring materials instead of synthetic, manufactured inputs.
Use on-farm resources as much as possible.
Recycle on-farm nutrients.
2. Minimize Toxics Reduce or eliminate the use of materials that have the potential to harm the environment or the health of
farmers, farm workers, or consumers.
Use farming practices that reduce or eliminate environmental pollution with nitrates, toxic gases, or other
materials generated by burning or overloading agro ecosystems with nutrients.
3. Conserve Resources
a. Conserve Soil Sustain soil nutrient and organic matter stocks.
Minimize erosion.
use perennials
Use no-till or reduced tillage methods.
Mulch.
b. Conserve Water Use efficient irrigation systems.
c. Conserve Energy
Use energy efficient technologies.
d. Conserve genetic resources
Save seed.
e. Conserve Capital
Keep bank debt to a minimum.
Reduce expenditures.
4. Manage Ecological Relationships Reestablish ecological relationships that can occur naturally on the farm instead of reducing and simplifying
them.
Manage pests, diseases, and weeds instead of “controlling” them.
Use intercropping and cover cropping
Integrate Livestock
Enhance beneficial biota
free-living nitrogen fixers in soils
Enhance beneficial populations by breed and release programs.
Recycle Nutrients
Shift from through flow nutrient management to recycling of nutrients.
Return crop residues and manures to soils.
When outside inputs are necessary, sustain their benefits by recycling them.
Minimize Disturbance
Use reduced tillage or no-till methods.
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Use mulches.
Use perennials
5. Adjust to Local Environments Match cropping patterns to the productive potential and physical limitations of the farm landscape.
Adapt Biota
Adapt plants and animals to the ecological conditions of the farm rather than modifying the farm to
meet the needs of the crops and animals.
6. Diversify
Landscapes Maintain undisturbed areas as buffer zones.
Use contour and strip tillage.
Use rotational grazing.
7. Biota Intercrop.
Rotate crops.
Use poly culture.
Integrate animals in system.
Use multiple species of crops and animals on farm.
Use multiple varieties and landraces of crops and animals on farm.
8. Economics Avoid dependence on single crops/products.
Use alternative markets.
Organic markets.
Community Supported Agriculture
Add value to agricultural products.
Process foods before selling them.
Find alternative incomes.
Agro tourism
Avoid dependence on external subsidies
Use multiple crops to diversify seasonal timing of production over the year.
9. Empower People a. Ensure that local people control their development process.
b. Use indigenous knowledge
c. Promote multi-directional transfer of knowledge, as opposed to "top-down" knowledge transfer.
d. Teach experts and farmers to share knowledge, not "impose" it.
10. Engage in people-centric development.
11. Increase farmer participation.
e. Link farmers with consumers
12. Strengthen communities.
f. Encourage local partnerships between people and development groups.
g. Ensure intergenerational fairness.
13. Guarantee agricultural labor.
Ensure equitable labor relations for farm workers.
14. Teach principles of agro ecology & sustainability.
15. Manage Whole Systems 16. Use planning processes that recognize the different scales of agro ecosystems.
Landscapes
Households
Farms
Communities
Bioregions
Nations
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17. Minimize impacts on neighboring ecosystems.
18. Maximize Long-Term Benefits a. Maximize intergenerational benefits, not just annual profits.
b. Maximize livelihoods and quality of life in rural areas.
c. Facilitate generational transfers.
d. Use long-term strategies.
Develop plans that can be adjusted and reevaluated through time.
Incorporate long-term sustainability into overall agro ecosystem design and management.
Build soil fertility over the long-term.
Build soil organic matter.
19. Value Health Human Health
Cultural Health
Environmental Health
Value most highly the overall health of agro ecosystems rather than the outcome of a particular crop
system or season.
Eliminate environmental pollution by toxics and surplus nutrients.
Animal Health
Plant Health
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CHAPTER TWO
2.1: MAJOR AGRO-ECOLOGICAL ZONES OF THE WORLD AND ASSOCIATED FARMING SYSTEM
Description of Koppen and Thornwaith’s methods of climatic classification
A, Koppen’s methods of climatic classification
Köppen climate classification widely used vegetation-based empirical climate classification system developed by
German botanist-climatologist Wladimir Köppen. His aim was to devise formulas that would define climatic
boundaries in such a way as to correspond to those of the vegetation zones (biomes) that were being mapped for the
first time during his lifetime. Köppen published his first scheme in 1900 and a revised version in 1918. He continued
to revise his system of classification until his death in 1940. Other climatologists have modified portions of
Köppen’s procedure on the basis of their experience in various parts of the world.
Köppen’s classification is based on a subdivision of terrestrial climates into five major types, which are represented
by the capital letters A, B, C, D, and E. Each of these climate types except for B is defined by temperature criteria.
Type B designates climates in which the controlling factor on vegetation is dryness (rather than coldness). Aridity is
not a matter of precipitation alone but is defined by the relationship between the precipitation input to the soil in
which the plants grow and the evaporative losses. Since evaporation is difficult to evaluate and is not a conventional
measurement at meteorological stations, Köppen was forced to substitute a formula that identifies aridity in terms of
a temperature-precipitation index (that is, evaporation is assumed to be controlled by temperature).
The Köppen Climate Classification System is the most widely used system for classifying the world's climates. Its
categories are based on the annual and monthly averages of temperature and precipitation. The Köppen system
recognizes five major climatic types; each type is designated by a capital letter.
A - Tropical Moist Climates: all months have average temperatures above 18° Celsius.
B - Dry Climates: with deficient precipitation during most of the year.
C - Moist Mid-latitude Climates with Mild Winters.
D - Moist Mid-Latitude Climates with Cold Winters.
E - Polar Climates: with extremely cold winters and summers.
Further subgroups are designated by a second, lower case letter which distinguishes specific seasonal characteristics
of temperature and precipitation.
f - Moist with adequate precipitation in all months and no dry season. This letter usually accompanies the A,
C, and D climates.
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m - Rainforest climate in spite of short, dry season in monsoon type cycle. This letter only applies to A
climates.
s - There is a dry season in the summer of the respective hemisphere (high-sun season).
w - There is a dry season in the winter of the respective hemisphere (low-sun season).
To further denote variations in climate, a third letter was added to the code.
a - Hot summers where the warmest month is over 22°C (72°F). These can be found in C and D climates.
b - Warm summer with the warmest month below 22°C (72°F). These can also be found in C and D
climates.
c - Cool, short summers with less than four months over 10°C (50°F) in the C and D climates.
d - Very cold winters with the coldest month below -38°C (-36°F) in the D climate only.
h - Dry-hot with a mean annual temperature over 18°C (64°F) in B climates only.
k - Dry-cold with a mean annual temperature under 18°C (64°F) in B climates only.
1. Tropical Moist Climates (A)
Tropical moist climates extend northward and southward from the equator to about 15 to 25° of latitude. In these
climates all months have average temperatures greater than 18° Celsius. Annual precipitation is greater than 1500
mm. Three minor Köppen climate types exist in the A group, and their designation is based on seasonal distribution
of rainfall.
Af or tropical wet is a tropical climate where precipitation occurs all year long. Monthly temperature
variations in this climate are less than 3° Celsius. Because of intense surface heating and high humidity,
cumulus and cumulonimbus clouds form early in the afternoons almost every day. Daily highs are about 32°
Celsius, while night time temperatures average 22° Celsius.
Am a tropical monsoon climate. Annual rainfall is equal to or greater than Af, but most of the precipitation
falls in the 7 to 9 hottest months. During the dry season very little rainfall occurs.
The tropical wet and dry or savanna (Aw) has an extended dry season during winter. Precipitation during
the wet season is usually less than 1000 millimeters, and only during the summer season.
2. Dry Climates (B)
The most obvious climatic feature of this climate is that potential evaporation and transpiration exceed precipitation.
These climates extend from 20 - 35° North and South of the equator and in large continental regions of the mid-
latitudes often surrounded by mountains. Minor types of this climate include:
BW - dry arid (desert) is a true desert climate. It covers 12% of the Earth's land surface and is dominated
by xerophytic vegetation. The additional letters h and k are used generally to distinguish whether the dry
arid climate is found in the subtropics or in the mid-latitudes, respectively.
BS - dry semiarid (steppe). Is a grassland climate that covers 14% of the Earth's land surface? It receives
more precipitation than the BW either from the inter tropical convergence zone or from mid-latitude
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cyclones. Once again, the additional letters h and k are used generally to distinguish whether the dry
semiarid climate is found in the subtropics or in the mid-latitudes, respectively.
3. Moist Subtropical Mid-Latitude Climates (C)
This climate generally has warm and humid summers with mild winters. Its extent is from 30 to 50° of latitude
mainly on the eastern and western borders of most continents. During the winter, the main weather feature is the
mid-latitude cyclone. Convective thunderstorms dominate summer months. Three minor types exist:
Cfa - humid subtropical;
Cs - Mediterranean; and
Cfb - marine.
The humid subtropical climate (Cfa) has hot muggy summers and frequent thunderstorms. Winters are mild and
precipitation during this season comes from mid-latitude cyclones. A good example of a Cfa climate is the
southeastern USA.
Cfb marine climates are found on the western coasts of continents. They have a humid climate with short dry
summer. Heavy precipitation occurs during the mild winters because of the continuous presence of mid-latitude
cyclones.
Mediterranean climates (Cs) receive rain primarily during winter season from the mid-latitude cyclone. Extreme
summer aridity is caused by the sinking air of the subtropical highs and may exist for up to 5 months. Locations in
North America are from Portland, Oregon to all of California.
4. Moist Continental Mid-latitude Climates (D)
Moist continental mid-latitude climates have warm to cool summers and cold winters. The location of these climates
is pole ward of the C climates. The average temperature of the warmest month is greater than 10° Celsius, while the
coldest month is less than -3° Celsius. Winters are severe with snowstorms, strong winds, and bitter cold from
Continental Polar or Arctic air masses. Like the C climates there are three minor types:
Dw - dry winters;
Ds - dry summers; and
Df - wet all seasons.
5. Polar Climates (E)
Polar climates have year-round cold temperatures with the warmest month less than 10° Celsius. Polar climates are
found on the northern coastal areas of North America, Europe, Asia, and on the landmasses of Greenland and
Antarctica. Two minor climate types exist.
ET or polar tundra is a climate where the soil is permanently frozen to depths of hundreds of meters, a
condition known as permafrost. Vegetation is dominated by mosses, lichens, dwarf trees and scattered
woody shrubs.
EF or polar ice caps has a surface that is permanently covered with snow and ice.
B, Thornwaith’s methods of climatic classification
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In 1931 Thornthwaite devised a complex and empirical classification, which is very close to Koppen's scheme. It
also attempts to define climatic boundaries quantitatively and is based on plant associations. However,
Thornthwaite's classification is based on precipitation effectiveness and thermal efficiency (temperature efficiency).
Under this classification climatic types were subdivided by the use of a term to denote the seasonal distribution of
precipitation. The climatic types and their boundaries were defined empirically by observing the characteristics of
natural vegetation, soil, and the drainage pattern.
Thornthwaite established the fact that not only the amount of precipitation, but the rate of evaporation as well is
significant for the growth of natural vegetation. Thus, besides the precipitation amount and the evaporation rate,
temperature was made a very important basis for Thornthwaite's climatic classification. An expression for
precipitation efficiency was obtained by relating measurements of pan evaporation to temperature and precipitation.
For each month the ratio 11.5 (rt-10)10/9 where r=mean monthly rainfall (in inches) t=mean monthly temperature (in
°F) is calculated.
The sum of the 12 monthly ratios gives the precipitation effectiveness (also called precipitation efficiency) index. In
other words, the effectiveness of precipitation is taken to be a function of precipitation and evaporation and is
calculated by dividing the monthly precipitation by the monthly evaporation to get the P/E ratio (precipitation
effectiveness ratio).
On the basis of P/E indices and boundary values for the major vegetation regions, five humidity provinces were
defined. Main Climatic groups based on precipitation effectiveness
Humidity Province Vegetation P/E Index
3. A (Wet) Rain Forest 127
4. B (Humid) Forest 64-127
5. C (Sub humid) Grassland 32-63
6. D (Semiarid) Steppe 16-31
7. E (Arid) Desert 16
Thornthwaite introduced an index of thermal efficiency which is expressed by the positive departure of monthly
mean temperatures from the freezing point. The index is thus the annual sum of (t-32)/4 for each month. In other
words, the sum of twelve monthly temperature-efficiency ratios (T/E) gives a T/E index
Again, the world was divided into 6 temperature provinces on the basis of T/E index. Main Climatic groups based on
thermal efficiency
Temperature Province T/E index
A-Tropical 127
B-Mesothermal 64-127
C-Microthermal 32-63
D-Taiga 16-31
E-Tundra 1-15
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F-Frost 0
T/E Index-sum of 12 monthly values of (T-32)14, where T is mean monthly temperature in °;F.
On the basis of the seasonal distribution of precipitation the humidity provinces were subdivided into the following
r-Rainfall adequate in all seasons
s-Rainfall deficient in summer
w-Rainfall deficient in winter
d-Rainfall deficient in all seasons.
When precipitation effectiveness, seasonal distribution of rainfall, and thermal efficiency are taken together, there
would be in all 120 climatic types, at least on theoretical grounds. However, Thornthwaite has shown only 32
climatic types on the world map depicting his 1931 climatic classification.
World climatic Types
Based on the above classification there are three basic climate groups found in the world. These three major climate
groups show the dominance of special combinations of air-mass source regions.
Group I, Low-latitude Climates:
These climates are controlled by equatorial a tropical air masses.
Tropical Moist Climates (Af) rainforest
Rainfall is heavy in all months. The total annual rainfall is often more than 250 cm. (100 in.). There are seasonal
differences in monthly rainfall but temperatures of 27°C (80°F) mostly stay the same. Humidity is between 77 and
88%. High surface heat and humidity cause cumulus clouds to form early in the afternoons almost every day. The
climate on eastern sides of continents is influenced by maritime tropical air masses. These air masses flow out from
the moist western sides of oceanic high-pressure cells, and bring lots of summer rainfall. The summers are warm and
very humid. It also rains a lot in the winter
Average temperature: 18 °C (°F)
Annual Precipitation: 262 cm. (103 in.)
Latitude Range: 10° S to 25 ° N
Global Position: Amazon Basin; Congo Basin of equatorial Africa; East Indies, from Sumatra to New Guinea.
Wet-Dry Tropical Climates (Aw) savanna
A seasonal change occurs between wet tropical air masses and dry tropical air masses. As a result, there is a very wet
season and a very dry season. Trade winds dominate during the dry season. It gets a little cooler during this dry
season but will become very hot just before the wet season.
Temperature Range: 16 °C
Annual Precipitation: 0.25 cm. (0.1 in.). All months less than 0.25 cm. (0.1 in.)
Latitude Range: 15 ° to 25 ° N and S
Global position: India, Indochina, West Africa, southern Africa, South America and the north coast of Australia
Dry Tropical Climate (BW) desert biome
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These desert climates are found in low-latitude deserts approximately between 18° to 28° in both hemispheres. these
latitude belts are centred on the tropics of Cancer and Capricorn, which lie just north and south of the equator. They
coincide with the edge of the equatorial subtropical high pressure belt and trade winds. Winds are light, which allows
for the evaporation of moisture in the intense heat. They generally flow downward so the area is seldom penetrated
by air masses that produce rain. This makes for a very dry heat. The dry arid desert is a true desert climate, and
covers 12 % of the Earth's land surface.
Temperature Range: 16° C
Annual Precipitation: 0.25 cm (0.1 in). All months less than 0.25 cm (0.1 in).
Latitude Range: 15° - 25° N and S.
Global position: south western United States and northern Mexico; Argentina; north Africa; south Africa; central part
of Australia.
Group II, Mid-latitude Climates:
Climates in this zone are affected by two different air-masses. The tropical air-masses are moving towards the poles
and the polar air-masses are moving towards the equator. These two air masses are in constant conflict. Either air
mass may dominate the area, but neither has exclusive control.
Dry Midlatitude Climates (BS) steppe
Characterized by grasslands, this is a semiarid climate. It can be found between the desert climate (BW) and more
humid climates of the A, C, and D groups. If it received less rain, the steppe would be classified as an arid desert.
With more rain, it would be classified as a tallgrass prairie. This dry climate exists in the interior regions of the North
American and Eurasian continents. Moist ocean air masses are blocked by mountain ranges to the west and south.
These mountain ranges also trap polar air in winter, making winters very cold. Summers are warm to hot.
Temperature Range: 24° C (43° F).
Annual Precipitation: less than 10 cm (4 in) in the driest regions to 50 cm (20 in) in the moister steppes.
Latitude Range: 35° - 55° N.
Global poasition: Western North America (Great Basin, Columbia Plateau, Great Plains); Eurasian interior, from
steppes of eastern Europe to the Gobi Desert and North China.
Mediterranean Climate (Cs) chaparral biome
This is a wet-winter, dry-summer climate. Extremely dry summers are caused by the sinking air of the subtropical
highs and may last for up to five months. Plants have adapted to the extreme difference in rainfall and temperature
between winter and summer seasons. Sclerophyll plants range in formations from forests, to woodland, and scrub.
Eucalyptus forests cover most of the chaparral biome in Australia. Fires occur frequently in Mediterranean climate
zones.
Temperature Range: 7 °C (12 °F)
Annual Precipitation: 42 cm (17 in).
Latitude Range: 30° - 50° N and S
UoG Dept of GeES
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Global Position: central and southern California; coastal zones bordering the Mediterranean Sea; coastal Western
Australia and South Australia; Chilean coast; Cape Town region of South Africa.
Dry Midlatitude Climates (Bs) grasslands biome
These dry climates are limited to the interiors of North America and Eurasia. Ocean air masses are blocked by
mountain ranges to the west and south. This allows polar air masses to dominate in winter months. In the summer, a
local continental air mass is dominant. A small amount of rain falls during this season. Annual temperatures range
widely. Summers are warm to hot, but winters are cold.
Temperature Range: 31 °C (56°F).
Annual Precipitation: 81 cm. (32 in.).
Latitude Range: 30° - 55° N and S
Global Position: western North America (Great Basin, Columbia Plateau, Great Plains); Eurasian interior.