Drought
is a period or condition of unusually dry weather within a geographic area
where rainfall is normally present. Droughts occur in all climatic zones.
However, its characteristics vary significantly from one region to another.
Drought usually results in a water shortage that seriously interferes with
human activity. Water-supply reservoirs empty, wells dry up, and crop damage
ensues. Its seriousness depends on the degree of the water shortage, size of
area affected, and the duration and warmth of the dry period.
CAUSES
1. Water
vapor condenses only if air rises into the colder regions of the atmosphere. If
the air doesn’t rise, then no rain will form. When there is high air pressure,
air falls instead of rising. With the air pressing down in a high pressure
zone, no currents of water vapor are carried upward. As a result, no
condensation occurs, and little rain falls to earth.
2. Most
precipitation depends on water vapor carried by winds from an ocean or other
source of moisture. If these moisture-carrying winds are replaced by winds from
a dry region or flow in different directions, the weather is abnormally dry and
often persistently cloudless.
3. Mountains
can prevent wind from blowing moisture to needed regions. As air is moving past
a mountain range, it is forced to rise in order to pass over the peaks.
However, as the air rises, it becomes colder and the vapor condenses into rain
or snow. The rain then falls on that side of the mountain, known as the
windward side (the side that is turned toward the wind). When the air mass
finally makes it over the mountain, it has lost much of its vapor. This is
another reason why many deserts are found on the side of a mountain facing away
from the ocean. This phenomenon is known as the rain shadow effect.
IMPACTS
a) Environmental:
- Some direct impacts of drought are reduced crop and forest productivity,
reduced ground water levels, increased fire hazard, increased livestock and
wildlife death rates, and damage to wildlife and fish habitat. Drought is also
associated with increases in insect infestations and plant disease. Forest
fires increase dramatically during periods of droughts.
b) Economic:
- A reduction in crop productivity usually results in less income for farmers,
increased prices for food, unemployment, and migration.
c) Social:
- Social impacts include health, public safety, conflicts between water users,
and reduced quality of life. During droughts many people migrate to areas
outside the drought-affected location. When this happens, the area loses a
great deal of its population, and thus the area has less financial support.
Between 1950 and 1980 the drought of Brazil had a loss of 5.5 million people.
This continues to be a significant problem in the economic development of
Brazil.
WARNING
AND DISSEMINATION
There
is a "Weather-Watch-Group" in the Ministry of Agriculture, which
meets every week to take stock of the rainfall progress, its effects on the
crops from sowing to harvesting, during the kharif season. Weekly input gives
an early warning about the impending drought as and when symptoms arise in this
regard and the states are warned accordingly. The drought assessment is based
on a comparative evaluation of satellite observed green vegetation cover (both
area and greenness) of a district in any specific time period, with that of any
similar period in previous years.
PREVENTION
Although
drought cannot be reliably predicted, certain precautions can be taken in
drought-risk areas. It is important to develop strategies to protect from
drought. Strategies for drought protection, mitigation or relief include:
1.
Construction of Dams:
The
construction of dams is a better choice to avoid drought. Dams work by storing
the extra water when it is available, so that during a time of drought, it can
be released. It is done both to prevent drought and to prevent flooding. The
main purpose of most dams is to create a permanent reservoir of water for use
at a later time. The dam must be watertight (i.e. impermeable or impervious to
water) so that water does not leak out of the dam and escape downstream. An
essential part of a dam is therefore the "impermeable membrane", i.e.
the watertight part of the dam that prevents water leaking out.
2.
Cloud seeding:
Cloud
seeding is the process of spreading either dry ice, or more commonly, silver
iodide aerosols, into the upper part of clouds to try to stimulate the
precipitation process and form rain. Since most rainfall starts through the
growth of ice crystals from super-cooled cloud droplets (droplets colder than
the freezing point, 32 deg. F or 0 deg. C) in the upper parts of clouds, the
silver iodide particles are meant to encourage the growth of new ice particles.
The history of cloud seeding has experienced uncertain results because it can
never be known whether a cloud that rains after seeding might have rained
anyway. This is because seeding is performed on clouds that look like they have
some potential for producing rain.
3.
Desalination:
It is
the process of removing soluble salts from water to render it suitable for drinking,
irrigation, or industrial uses. The principal methods used for desalination
include distillation (or evaporation), electro dialysis, freezing, ion
exchange, and reverse osmosis.
4.
Rainwater Harvesting:
Broadly
rainwater can be harvested for two purposes
· Storing
rainwater for ready use in containers above and below ground.
· Charged
into soil for withdrawal later.
Rainwater
harvesting can be harvested from the following surfaces
Roofftops.
Paved and
unpaved areas.
· Water
bodies.
Storm
water drains.
The
decision whether to store or recharge water depends on the rainfall pattern and
the potential to do so, in a particular region. The sub-surface geology also
plays an important role in making this decision.
5.
Recycled water:
The use
of recycled water in horticulture (urban and rural) and industry, as well as in
residential areas has grown considerably over the past decade. Recycled water
is water from the city or sewage that is then treated and reused. No potable
water, not suited for drinking, is reused on a daily basis in some cities. It
can be used for such things as car washes, laundry facilities, road cleaning,
firefighting and toilet flushing. No potable water reuse is most beneficial in
cities when irrigation is in full swing at ball fields, golf courses, parks,
schoolyards and residential lawns. Using reclaimed water for irrigation has a
marked difference on potable water levels during these months.
6.
Other small scale methods:
a.
Mulching
Mulches
like UV stabilized poly-sheets have become the major input for growing crops.
Such sheets reflect the sunlight and causes minimum soil moisture evaporation.
Israel is the leading country adopting this method with very high productivity.
b.
Coconut Compost
India
has plenty of resources to tackle soil moisture retention like the coconut
compost. When the coconut husk is composted and added to soil, the coconut
fibre absorbs moisture from the soil and retails for a long period releasing
moisture gradually to crops. This technology has made farming in drought prone
areas very simple. Many coconut husk processing units in Tamil Nadu like
Pollachi is taking advantage and exports several thousand tons of coconut
compost to countries like Israel which uses as a media in green houses for
growing roses, vegetables and fruits.
c.
Water Aquifers
Water
aquifers are made to recharge the ground water without wasting the rain water.
Aquifers are simple methods of percolation by which small bore wells are dug
and the inner surface is perforated and filled with gravel to absorb the rain
water. The rain water percolates deep into the ground and recharges the ground
water.
FAMOUS
DROUGHTS
1. When
pioneers headed west in the late 19th century, many couldn't resist the lure
of the tall grassy land in the semiarid midwestern and southern plains of the
United States. They settled there to farm. They were prosperous in the decades
that followed, but when the 1930s rolled in, so did strong winds, drought and
clouds of dust that plagued nearly 75 percent of the United States between 1931
and 1939 [source: PBS]. The era became known as the legendary Dust Bowl. The
Dust Bowl brought ecological, economical and human misery to America during a
time when it was already suffering under the Great Depression.
2. There
was a major drought in the Sahel, Africa in 1914, caused by annual rains far
below average that caused a large-scale famine. As another long drought-period
from 1968 through 1974 began, the grazing quickly became unsustainable, and
large-scale denuding of the terrain followed. Like the drought in 1914, this
led to a large-scale famine, but this time it was somewhat tempered by
international visibility and an outpouring of aid. This catastrophe led to the
founding of the International Fund for Agricultural Development. In June to
August, 2010, famine struck the Sahel again. Niger's crops failed to mature in
the heat, and famine occurred. 350,000 faced starvation, and 1,200,000 were at
risk of famine.