Jawahar Navodaya Vidyalaya
Topic- Disaster Management
Balod, (C.G.)
Geography project
Made by Guided by
Aayush Uike Mr. S.K. Singh
(Pgt.Geography)
This Photo by Unknown author is licensed under CC BY-NC.
(Drought)
Contents
• What is Disaster management ?
• Mitigation, Preparedness & Response
• Types of Drought
• Meteorological drought
• Agricultural drought
• Hydrological drought
• Causes of drought
• Protection mitigation and relief
What is Disaster
management ?
Disaster Management can be defined
as the organization
and management of resources and
responsibilities for dealing with all
humanitarian aspects of
emergencies, in particular
preparedness, response and
recovery in order to lessen the
impact of disasters.
Mitigation, Preparedness & Response
Drought mitigation, preparedness and response comprise the
appropriate measures and actions aimed at reducing the
vulnerability to drought and reducing the impacts of droughts. The goal
of the pillar on drought mitigation, preparedness and response is to
determine appropriate mitigation and response actions aimed at risk
reduction, the identification of appropriate triggers to phase in and
phase out mitigation actions, particularly short-term actions, during
drought onset and termination and, finally, to identify agencies or
ministries or organizations to develop and implement mitigation
actions.
Types of Drought
Drought is mainly defined in three
ways:-
i) Meteorological drought
ii) Agricultural drought
iii) Hydrological drought
Meteorological drought
Meteorological drought occurs
when there is a prolonged time
with less than average
precipitation. Meteorological
drought usually precedes the
other kinds of drought.
Agricultural Drought
Agricultural droughts affect crop
production or the ecology of the range.
This condition can also arise
independently from any change in
precipitation levels when either
increased irrigation or soil conditions and
erosion triggered by poorly planned
agricultural endeavors cause a shortfall in
water available to the crops. However, in
a traditional drought, it is caused by an
extended period of below average
precipitation
Hydrological drought
Hydrological drought is brought about
when the water reserves available in
sources such
as aquifers, lakes and reservoirs fall
below a locally significant threshold.
Hydrological drought tends to show up
more slowly because it involves stored
water that is used but not replenished.
Like an agricultural drought, this can
be triggered by more than just a loss
of rainfall
Causes of drought
Precipitation deficiency
Mechanisms of producing precipitation
include convective, stratiform, and orographic rai
nfall. Convective processes involve strong
vertical motions that can cause the overturning
of the atmosphere in that location within an hour
and cause heavy precipitation, while stratiform
processes involve weaker upward motions and
less intense precipitation over a longer
duration.]Precipitation can be divided into three
categories, based on whether it falls as liquid
water, liquid water that freezes on contact with
the surface, or ice. Droughts occur mainly in
areas where normal levels of rainfall are, in
themselves, low. If these factors do not support
precipitation volumes sufficiently to reach the
surface over a sufficient time, the result is a
drought.
Temperature
increases
Evaporation
increases
Ground dries
Dry season
Within the tropics, distinct, wet and
dry seasons emerge due to the
movement of the Intertropical
Convergence Zone or Monsoon trough.
The dry season greatly increases drought
occurrence, and is characterized by its
low humidity, with watering holes and
rivers drying up. Because of the lack of
these watering holes, many grazing
animals are forced to migrate due to the
lack of water in search of more fertile
lands.
This Photo by Unknown author is licensed under CC BY-NC-ND.
Erosion and human
activities
Human activity can directly trigger exacerbating
factors such as over farming, excessive irrigation
deforestation, and erosion adversely impact the
ability of the land to capture and hold water. In arid
climates, the main source of erosion is
wind. Erosion can be the result of material
movement by the wind. The wind can cause small
particles to be lifted and therefore moved to
another region (deflation). Suspended particles
within the wind may impact on solid objects
causing erosion by abrasion (ecological
succession). Wind erosion generally occurs in
areas with little or no vegetation, often in areas
where there is insufficient rainfall to support
vegetation.
Climatic changes
Overall, global warming will result in increased
world rainfall. Activities resulting in
global climate change are expected to trigger
droughts with a substantial impact on
agriculture throughout the world, and
especially in developing nations. Along with
drought in some areas, flooding and erosion
could increase in others. Some
proposed solutions to global warming that
focus on more active techniques, solar
radiation management through the use of
a space sunshade for one, may also carry
with them increased chances of drought.[
Consequences of drought
One can divide the effects of droughts and water
shortages into three groups: environmental, economic and
social.
• In the case of environmental effects: lower surface and
subterranean water-levels, lower flow-levels (with a
decrease below the minimum leading to direct danger for
amphibian life), increased pollution of surface water, the
drying out of wetlands, more and larger fires, higher
deflation intensity, loss of biodiversity, worse health of
trees and the appearance of pests and dendroid
diseases.
• Economic losses include lower agricultural, forests, game
and fishing output, higher food-production costs, lower
energy-production levels in hydro plants, losses caused
by depleted water tourism and transport revenue,
problems with water supply for the energy sector and for
technological processes in metallurgy, mining, the
chemical, paper, wood, foodstuff industries etc., disruption
of water supplies for municipal economies.
Protection, mitigation and relief
• Dams – many dams and their associated reservoirs supply additional water in times of
drought.
• Cloud seeding – a form of intentional weather modification to induce rainfall. This remains
a hotly debated topic, as the United States National Research Council released a report in
2004 stating that to date, there is still no convincing scientific proof of the efficacy of
intentional weather modification.[
• Rainwater harvesting – Collection and storage of rainwater from roofs or other suitable
catchments.
• Recycled water – Former wastewater (sewage) that has been treated and purified for reuse.
• Transvasement – Building canals or redirecting rivers as massive attempts at irrigation in
drought-prone areas.
Thank You

Powerpoint on Drought (Geography) USacademy.in

  • 1.
    Jawahar Navodaya Vidyalaya Topic-Disaster Management Balod, (C.G.) Geography project Made by Guided by Aayush Uike Mr. S.K. Singh (Pgt.Geography) This Photo by Unknown author is licensed under CC BY-NC. (Drought)
  • 2.
    Contents • What isDisaster management ? • Mitigation, Preparedness & Response • Types of Drought • Meteorological drought • Agricultural drought • Hydrological drought • Causes of drought • Protection mitigation and relief
  • 3.
    What is Disaster management? Disaster Management can be defined as the organization and management of resources and responsibilities for dealing with all humanitarian aspects of emergencies, in particular preparedness, response and recovery in order to lessen the impact of disasters.
  • 4.
    Mitigation, Preparedness &Response Drought mitigation, preparedness and response comprise the appropriate measures and actions aimed at reducing the vulnerability to drought and reducing the impacts of droughts. The goal of the pillar on drought mitigation, preparedness and response is to determine appropriate mitigation and response actions aimed at risk reduction, the identification of appropriate triggers to phase in and phase out mitigation actions, particularly short-term actions, during drought onset and termination and, finally, to identify agencies or ministries or organizations to develop and implement mitigation actions.
  • 5.
    Types of Drought Droughtis mainly defined in three ways:- i) Meteorological drought ii) Agricultural drought iii) Hydrological drought
  • 6.
    Meteorological drought Meteorological droughtoccurs when there is a prolonged time with less than average precipitation. Meteorological drought usually precedes the other kinds of drought.
  • 7.
    Agricultural Drought Agricultural droughtsaffect crop production or the ecology of the range. This condition can also arise independently from any change in precipitation levels when either increased irrigation or soil conditions and erosion triggered by poorly planned agricultural endeavors cause a shortfall in water available to the crops. However, in a traditional drought, it is caused by an extended period of below average precipitation
  • 8.
    Hydrological drought Hydrological droughtis brought about when the water reserves available in sources such as aquifers, lakes and reservoirs fall below a locally significant threshold. Hydrological drought tends to show up more slowly because it involves stored water that is used but not replenished. Like an agricultural drought, this can be triggered by more than just a loss of rainfall
  • 9.
    Causes of drought Precipitationdeficiency Mechanisms of producing precipitation include convective, stratiform, and orographic rai nfall. Convective processes involve strong vertical motions that can cause the overturning of the atmosphere in that location within an hour and cause heavy precipitation, while stratiform processes involve weaker upward motions and less intense precipitation over a longer duration.]Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice. Droughts occur mainly in areas where normal levels of rainfall are, in themselves, low. If these factors do not support precipitation volumes sufficiently to reach the surface over a sufficient time, the result is a drought. Temperature increases Evaporation increases Ground dries
  • 10.
    Dry season Within thetropics, distinct, wet and dry seasons emerge due to the movement of the Intertropical Convergence Zone or Monsoon trough. The dry season greatly increases drought occurrence, and is characterized by its low humidity, with watering holes and rivers drying up. Because of the lack of these watering holes, many grazing animals are forced to migrate due to the lack of water in search of more fertile lands. This Photo by Unknown author is licensed under CC BY-NC-ND.
  • 11.
    Erosion and human activities Humanactivity can directly trigger exacerbating factors such as over farming, excessive irrigation deforestation, and erosion adversely impact the ability of the land to capture and hold water. In arid climates, the main source of erosion is wind. Erosion can be the result of material movement by the wind. The wind can cause small particles to be lifted and therefore moved to another region (deflation). Suspended particles within the wind may impact on solid objects causing erosion by abrasion (ecological succession). Wind erosion generally occurs in areas with little or no vegetation, often in areas where there is insufficient rainfall to support vegetation.
  • 12.
    Climatic changes Overall, globalwarming will result in increased world rainfall. Activities resulting in global climate change are expected to trigger droughts with a substantial impact on agriculture throughout the world, and especially in developing nations. Along with drought in some areas, flooding and erosion could increase in others. Some proposed solutions to global warming that focus on more active techniques, solar radiation management through the use of a space sunshade for one, may also carry with them increased chances of drought.[
  • 13.
    Consequences of drought Onecan divide the effects of droughts and water shortages into three groups: environmental, economic and social. • In the case of environmental effects: lower surface and subterranean water-levels, lower flow-levels (with a decrease below the minimum leading to direct danger for amphibian life), increased pollution of surface water, the drying out of wetlands, more and larger fires, higher deflation intensity, loss of biodiversity, worse health of trees and the appearance of pests and dendroid diseases. • Economic losses include lower agricultural, forests, game and fishing output, higher food-production costs, lower energy-production levels in hydro plants, losses caused by depleted water tourism and transport revenue, problems with water supply for the energy sector and for technological processes in metallurgy, mining, the chemical, paper, wood, foodstuff industries etc., disruption of water supplies for municipal economies.
  • 14.
    Protection, mitigation andrelief • Dams – many dams and their associated reservoirs supply additional water in times of drought. • Cloud seeding – a form of intentional weather modification to induce rainfall. This remains a hotly debated topic, as the United States National Research Council released a report in 2004 stating that to date, there is still no convincing scientific proof of the efficacy of intentional weather modification.[ • Rainwater harvesting – Collection and storage of rainwater from roofs or other suitable catchments. • Recycled water – Former wastewater (sewage) that has been treated and purified for reuse. • Transvasement – Building canals or redirecting rivers as massive attempts at irrigation in drought-prone areas.
  • 15.