S. M. Kulshrestha*

India experiences a greater variety of
weather than perhaps any other region of similar size anywhere else in the
world. This is so not only because of the large size of the country nor simply
because India is located in the tropics although both these facts are
important. Nature has bestowed upon India a unique weather and climate system
that is significant from the scientific as well as socio- economic angles.
India’s unique weather and climate
system stems from the country’s peculiar geography. India, a country of sub-continental size and situated
between the latitudes 804’ N and 3706’ N and longitudes
6807’ E and 97025’ E, is the tropics largest peninsula in
the world and is surrounded by seas on the three sides with an extensive
coastline of about 6000 km. With the icy continent of Antarctica as its major
neighbour to the south with vast streatch of the Indian Ocean in between. India
has the world’s tallest wall (the Himalayas) on its northern boundary.
Adjoining the Himalayas further north, is the Tibetan plateau which is large,
massive and about 5 km high- a gigantic slab of rock protruding up to the
middle of the troposphere and acting as a large sized heat source at the mid-
tropospheric level.
India
is gifted with a river system involving over 20 major rivers with many
tributaries. Physiographically. India comprises seven regions, viz. (I)
Northern mountains (the Himalayas), (2) Indo-Gangetic plains, (3) Central
highlands, (4) Peninsular plateau, (5) East coast, (6) West coast, and (7) the
islands (Andaman & Nicobar Group in the Bay of Bengal and Lakshadweep group
in the Arabian Sea).
India’s
unique geographical configuration gives it the peculiar climate regime with two
monsoon seasons and two cyclone seasons interspersed with hot and cold weather
seasons which see considerable thunderstorm activity. The cyclone seasons in
the pre-monsoon months (April-May) and the post-monsoon months (October-
November) bring cyclonic storms causing large scale inundation, destruction and
deaths. The two monsoon seasons (the south west monsoon in June to September
and the northeast monsoon in November- December bring forth rains-many a times
in intensities and amounts sufficient to cause serious floods creating
hazardous (and often disastrous) situation. In fact, floods and cyclones are
the two major natural disasters which visit India quite often. The adverse
impacts of these two natural disasters cannot be assessed merely in rupee terms
based on destruction of crops, property and infrastructure because the toll of
human misery in the form of death, disease, injury, loss of employment,
psychological trauma, and above all the set-back to development are too
difficult to compute.
2. INDIA’S RAINFALL REGIME
At
this stage, it will be useful to have an appreciation of the rainfall regime of
the country as both these natural disasters (floods and cyclones) are rainfall
related.
The
long term average annual rainfall for the country as a whole is 116 cm- again
the highest for a land of comparable size in the world. But this rainfall is
highly variable both in time and space. The heaviest rains occur over the hilly
States in the northeast and along the mountainous west coast (the Western Ghats
and the Konkan coast). In contrast, southwest Rajasthan receives hardly 15 cm
in a year. The percentage areal distribution of annual rainfall over India is
indicated below.
Mean Annual
Rainfall Corresponding % Area
0-75
cm 30%
75-125 cm 42%
125-200 cm 20%
> 200 cm 8%
The
above data point to the areal or spatial variability of the Indian rainfall
regime. The rainfall is highly variable in time as well. The maximum rainfall
occurs in July and August during the four- month (June to September) southwest
monsoon season. There are considerable intra- seasonal as well as inter-
seasonal variations.
The
areal distribution pattern of rainy days (days with rainfall of 2.5 mm or more)
generally follows the rainfall distribution pattern indicated above. The
Western Ghats, the northeastern States, and sub-Himalayan West- Bengal have
more than 100 rainy days. In the extenreme west Rajasthan, the number of rainy
days is less than 10. In the northern plains, the number of rainy days
decreases from east to west. In the peninsular region of the country, the semi-
arid areas (from Madhya Mahrashtra to Tamil Nadu) have between 40 and 50 rainy
days on the average. The number of rainy days in the central parts of the
country comprising Orissa, Madhya Pradesh and the adjoining Andhra Pradesh
varies between 50 and 75.
The
seasonal distribution of rainfall over India is quite interesting. The
southwest monsoon season extending from June to September is the principal
rainy season and it accounts for about 80% of the annual rainfall of the
country as a whole. Even Tamil Nadu, which is regarded as a shadow zone during the southwest monsoon season,
receives almost 50% of its annual rainfall during the season. The post-monsoon
season (October and November) brings rains to peninsular India especially the east coast through the mechanism of
northeast monsoon and cyclonic storms. The winter season (December to February)
is characterized by occasional visits of cyclones to the more southern parts of
the country, and by western disturbances which given rain over northwest India,
particularly the States of Jammu & Kashmir, Punjab, Himachal Pradesh, the
hills of west Uttar Pradesh (Uttaranchal) and northern areas of Rajasthan. Then
follows the pre-monsoon (hot weather) season of March to May which brings
thunderstorm/ duststorm activity over east and north India and cyclonic storms to
peninsular India especially the coastal
areas.
3.
THE SOUTHWEST MONSOON
Since
the southwest monsoon is the principal rain giver for India, it is useful to
note that the following four mechanisms are responsible for the large
variability of the monsoon rainfall
a)
The commencement of
rains may be early or delayed over the whole country or a large part of it.
(Early or delayed onset of the monsoon)
b)
There may be
extended periods of no or little rain during the normally most active months of
July and August. (prolonged onset of the monsoon).
c)
Rains may end
considerably earlier than normal or may prolong. (Early or late withdrawal of
the monsoon)
d)
Rains may persist or
prolong unusually in one part of the country and shun other regions. (Erratic
distribution of the monsoon)
It
is the inherent variability of the rainfall over India, and particularly during
the monsoon season, both in time and space that makes India especially
vulnerable to floods.
4. FLOOD AND
CYCLONE DISASTERS
Floods
and cyclones are the natural disasters where excess of water (rains) creates
the havoc. In case of cyclones, the
wind fury and the inundation of coastal areas by the selfish sea water of the
accompanying storm surge add to the destruction and misery. In case of floods,
the swollen rivers with overflowing banks do the damage in flood plains. Of
late, flooding or water logging is becoming a major problem in urban and
metropolitan areas. Cyclonic storms pose a hazard mainly in coastal regions
(more on the east coast as compared to the west coast) but no place in the
country is free from floods (even Rajasthan suffers from floods and flooding)
although flood plains of rivers and cyclone- affected coastal regions are most
prone to floods. While cyclone is a natural disaster in the full sense of the
term, flood problem (including flooding) is seriously aggravated by human
activities such as overgrazing, deforestation, soil erosion siltation, and
thoughtless construction. It is worthy of note that on the average the area
actually affected by floods every year in the country is of the order of 10
million hectares of which about half is cropland. In fact, according to the
report of the Rastriya Barh Aayog, the area prone to floods in the country is
of the order of 40 million hectares and that estimate was made two decades ago.
It
is in this background that the forecasting and warning of floods and cyclones
assume great importance. But before describing the forecasting and warning
system operational in the country for dealing with floods and cyclones, it
would be advisable to understand the significance of the concepts of
predictability, forecasting and warning (and their inter- relationship) as
applicable to the natural disasters such as floods and cyclones.
5. PREDICTABILITY, FORECASTING, AND WARNING
AND THEIR INTER-RELATIONSHIP
As
has been brought out in the preceding Sections, the occurrence of flood and
cyclones is highly variable in time and space although there are preferred locations
(coasts for cyclones and riverine flood plains for floods) and seasons (monsoon
for floods and pre-monsoon and post-monsoon seasons for cyclones). Furthermore,
no two events are similar. When a flood or a cyclone recurs, it would certainly
differ in intensity, coverage, duration and impact. The variability is inherent
in the very nature of floods and cyclones. This is all the more the reason that
we should appreciate the concepts of predictability. Forecasting and warning in
the context of floods and cyclones.
Predictability
of a disaster is the key to understand its nature and thereby assess the
probability of its occurrence and the anticipated fury of the event. In the
sense, predictability is an attribute amply applicable to natural disasters
such as floods and cyclones. It has no relevance for natural disasters such as
earthquakes nor for man-made disasters such as industrial disasters where a
human error or a mechanical fault is responsible for turning a hazard into a
disaster.
In
case of floods, the predictability in practical terms pertains to that of heavy
monsoon rains at any place or time. There are additional aspects that need to be considered because these
determine whether a particularly heavy rainfall would result in floods or
flooding. For example, repeated or persistent occurrence of rainfall over an
area already soaked with rain will certainly result in flooding or flood.
Excess water in a river, due to heavy
and/ or persistent rains in the catchment area or the upper regions of
the river system will create flood downstream. Absence or lack of adequate
drainage in any area will aggravate the flooding. Hence the predictability of
floods hinges on, i) the predictability of rainfall (read predictability of
monsoon), ii) antecedent rain condition of the area, iii) whether a river or a
stream flowing through the area is bringing excess water from upstream regions,
and (iv) if there is a drainage problem resulting in accumulation of water in
the area. As all these aspects are either predictable in advance or
monitor-able in real time, it is reasonable to conclude that floods have a
reasonable good predictability.
Cyclones
have the best predictability among all the disaster phenomena. This is because
their formation (cyclogenesis) and subsequent behaviour are fairly well
understood. Furthermore, cyclones can be detected as soon as they form over
oceans and can be kept under continuous watch through meteorological satellites
and radars. The magnitude of the accompanying hazard of storm surge is also
predictable through techniques which take into account the parameters of the
approaching cyclone as well as the physical and oceanographic characteristics
of the coast in the area of anticipated landfall i.e. the place where the cyclone
is expected to hit the coast.
For
the natural disasters that possess a fair degree of inherent predictability
such as floods and cyclones, forecasting is the next step in disaster
reduction. But forecasting has to be based on sound scientific principles and
operationally proven techniques. Forecasting has to be done by an authorized
agency, institution or individual who, besides being competent, experienced,
responsible and accountable, is conscious of the end-use of the forecast, its implications,
and the dependence of the success of disaster reduction on the forecast. In
order to be effective, a forecast has to be worded clearly and unambiguously
and it has to reach the users as quickly as possible.
Flood
forecasting for rivers means basically that an estimate is made of the future
stages or water levels in the river at selected points along the river during
flood season. The aim is to forecast the crest and its time of occurrence at a
place along the river. For this, it is necessary to have the relevant
hydrological data such as the characteristics of the river basin and the flood
plains and hydro meteorological data like the rainfall in the catchment area,
weather forecast, current levels of water and flow in the river.
For
floods other than river floods such as flash floods, and water-logging due to
inadequate drainage, forecasting takes the shape of monitoring because
forecasting of such local events is not practical and the only effective method
is to mount a monitoring and reporting system locally.
Forecasting
of cyclones is quite well developed. The cyclone forecasters (meteorologists)
are able to detect the formation and subsequent movement of cyclones of weather
charts that they prepare regularly, either manually or computer- generated,
based on observations of atmospheric pressure, temperature, humidity and winds
near the earth’s surface and at different levels in the atmosphere.
Simultaneously they locate and track the cyclones through satellites and high
power cyclone detection radars. The image of cyclone from satellites and radars
enable a constant monitoring of the intensification or weakening of the
cyclone.
Even
then, forecasting of the movement of a cyclone and the landfall point, i.e.,
the place where it will hit the coast, is a highly skilled task. Cyclones do
not travel in straight lines. Their tracks are usually curved and cyclones
often make small loops as they go along. Cyclones do not maintain a constant
speed along their path. Sometimes they slow down or remain stationary or
suddenly increase their speed. Therefore a cyclone is kept under constant
surveillance and the forecast is frequently updated.
Once
a forecast is available regarding an anticipated disaster event, it has to be
converted quickly into an area-specific and time-specific warning. Furthermore,
the warnings also need to be user- specific because the capacity of different
users to withstand the onslaught of a disaster is different. For example, the
general warnings for the public would be different from those required
specifically for the safety of a railway bridge during cyclone conditions
because a strong structure such as a railway bridge is designed to withstand a
certain force of high winds and to permit a certain level of river water
buffeting it pylons. Warnings in this case need to be issued only if the anticipated cyclonic winds and river-flow
are expected to go beyond the specified safety thresholds. However for the
public, where houses of various types and strengths including the hutments in
low lying areas have to face the fury of cyclones and/or floods, the warnings
have to be in terms of the anticipated winds and rainfall in the hope that the
individuals and the communities will be prepared and take prompt action with
the help of government and non-government organizations wherever the
anticipated impacts are likely to be dangerous. It is important to emphasize
that a warning has no value unless it reaches the users quickly and well in
time. Therefore quick communication is very important at the warning stage.
The
inter-relationship between Predictability, Forecasting and Warning is
self-evident and would have been clear from the discussion in the preceding
paragraphs. To repeat, a warning can only be issued on the basis of a useful
forecast and a disaster can be forecast only if it has an inherent
predictability about it.
Event if an event is predictable, a useful forecast is available, the appropriate warning has been issued and it has reached the users in time; the whole exercise will be fruitful only if the warning is believed and acted upon by the users. Therefore credibility is very essential at every stage of the process of forecasting and warning. That is why the concerned agencies strive hard to build credibility for their forecasts and warnings so that users develop confidence in these and take required action immediately and effectively.
While it is not possible to prevent the
occurrence of natural disasters, it is certainly possible to reduce the
resultant disastrous effects through adequate preparedness and timely action.
The effectiveness of timely action is generally enhanced through accurate
forecasts and clearly worded prompt warnings. Herein lies the importance and
significance of forecasts and warnings of natural disasters such as floods and
cyclones.
The
significance of warnings is well summarized in the Manual of Disaster
Prevention and Mitigation, Preparedness Aspects issued by the United Nations
Disaster Relief Organization (now called the United Nations Department of
Humanitarian Affairs) which states:
“
It is axiomatic that if timely warning can be given of an impending or probable
event which may bring disastrous consequences in its train, then it will be
possible to reduce the severity of those consequences. The degree to which the
reduction can be effected will depend upon the interplay of three main elements
namely:
-
the accuracy of the
warning:
-
the length of time
between the warning being issued and the expected onset of the event; and
-
the state of
pre-disaster planning and readiness
Included
within this last element is a sub-element that is the degree to which the
public respond to the warning and take correct precautionary action”.
Therefore the credibility of a warning
is the touchstone of its effectiveness.
6. THE FLOOD
FORECASTING AND WARNING SYSTEM IN INDIA
Flood
forecasting and warning constitute a reliable and cost-effective (therefore
very important) non-structural measure for flood related disaster reduction.
Flood forecasting and warning involves two aspects viz., (i) heavy rainfall
forecasting and warning and (ii) river related flood forecasting and warning.
Heavy rainfall forecasts and warnings are issued by the India Meteorological
Department (IMD) on the basis of the prevailing meteorological conditions
(synoptic situation) taking into account the climatologic as well as the
intensity and persistence of the on-going rain-producing weather phenomena such
as troughs. Depressions and cyclones. Heavy rainfall forecasts and warnings
are also disseminated to the public
through radio, television and newspapers in the concerned area in local
language (s).
The
present day riverine flood forecasting and warning system in India has a 40 year
history dating back to the establishment of the first Flood Forecasting Station
at Delhi Railway Bridge on river Yamuna in 1958. The first
flood forecast was issued on 25 July 1959 for this station. Since then, the
flood forecasting organization of the Central Water Commission (CWC) has
expanded gradually to a network of 157 Flood Forecasting Stations located in 11
States and 2 Union Territories thus covering most of the major inter-State
rivers in the country. Bihar, being the most flood prone state, has
the largest number of Flood Forecasting
Stations followed by other States and Union Territories as indicated below.
|
Bihar |
36 |
|
Uttar Pradesh |
33 |
|
Assam |
23 |
|
West Bengal |
14 |
|
Orissa |
11 |
|
Andhra Pradesh |
11 |
|
Gujarat |
10 |
|
Maharashtra |
7 |
|
Karnataka |
4 |
|
Madhya Pradesh |
3 |
|
Delhi |
2 |
|
Dadra & Nagar Haveli |
2 |
|
Haryana |
1 |
On the average, about 6000 flood forecasts are issued annually- most of these during the monsoon months. Flood forecasts are issued daily between May and October in order to take care of likely floods due to cyclones and monsoon rains. As in the case of dissemination of heavy rainfall forecasts and warnings by IMD, the flood forecasts from CWC are addressed to the specific users including the State Governments and District authorities and are made public through electronic and print media. Flood forecasts, in the form of computer generated daily bulletin from CWC, are also made available in all the district through NICNET, the countrywide computer network of the National Informatics Centre (NIC) of the Government of India.
The
warning responsibility in case of floods is taken up by the State Governments
and their District Administrations. The State governments, based on the local
experience, fix ”Danger Levels” for a river at vulnerable places such as near
cities or bridges. If the local conditions change, the “Danger Level” can be
refixed. CWC issues flood forecast when the river level at a given place
reaches or is expected to reach the “Warning Level” which is usually one meter
below the “Danger Level”. CWC issues flood forecasts in the form of “Daily
Water Level and Flood Forecast Bulletin”. During flood seasons. State
governments set up Control Rooms at the State and District Flood Forecast
Bulletin”. During flood seasons, State Governments set up Control Rooms at the
State and District Headquarters which receive the forecasts from the Flood
Forecasting Stations of CWC, convert these into place-specific warnings to the
relevant locations and also take appropriate action. The warnings are regularly
updated as new observations and forecasts are received.
The
inputs to the flood forecasting system come from the field observational
networks of the two agencies of Central Government viz., the India
Meteorological Department (IMD) and the Central Water Commission (CWC) although
the nodal agency for formulating flood forecasts is the Central Water
Commission (CWC). The meteorological inputs to the system are provided by the
Food Meteorological Officers (FMO) network of IMD.
Flood forecast formulation procedures involve collection of hydrological and hydro meteorological data. Past data are utilized for development / refinement of flood forecasting techniques. The forecast at a Flood Forecasting Station is generally formulated for river stage and its time of occurrence. For reservoir regulation, forecast is given for inflow and its distribution in time. For formulating flood forecasts, various graphical techniques, rainfall-fun off models, application of unit hydrograph, and computer modeling methods are used.
In summary, the flood forecasting
system of CWC involves the following steps:
i) Hydrological
and hydrometeorological observations at the field networks of CWC and IMD.
i)
Transmission
of data from field to Flood Forecasting Station (via IMD’s Flood Meteorological
Offices in case of Hydrometeorological data.)
ii)
Data
processing and formulation of flood forecast at CWC’s Flood Forecasting
Stations.
iii)
Dissemination
of flood forecasts to users.
iv)
Flood
forecast monitoring and evaluation.
The
last step i.e., monitoring and evaluation of flood forecasts is a very
significant step and CWC attaches great importance to it. For this purpose and
to ensure unbiased evaluation, a software package FFWNPAS (Flood Forecasting
and Warning Network Performance Appraisal) has been developed. This software
package is capable of evaluating the performance of CWC’s Flood Forecasting
Stations Network as well as on-line
monitoring of any unusual flood situation by producing a hydrograph.
According
to the norms followed by CWC, a flood forecast is considered to be reasonably
accurate if the difference between the forecast level and the corresponding
actual level of the river at the forecast place and time is within + 15
cm. Forecast accuracy performance based on this criterion is assessed for each
forecast issued from the network of flood forecasting stations and later CWC
evaluates the overall performance of the flood forecasting system as a whole.
The performance of the past years has been well documented and published by CWC
every year since 1986. An overall accuracy of 90-95% has been claimed for the
flood forecasts which means that 90-95% of the flood forecasts satisfy the
accuracy criterion mentioned above.
The
existing flood forecasting system provides macro scale service only. As
structured at present, the system does not cater to remote areas (such as small
communities in the hills) and basins served by small streams. But such areas do
have recurrent flood problem. Moreover such communities are often economically
disadvantaged. General wide area forecasts of heavy rain result in apathy or
over action and credibility suffers.
Flash floods in mountainous areas result mostly after a temporary blockage of
natural flow of rain or stream water. Here local detection and timely action
through a system of community volunteer watch seems to be the answer and such a
system should be mounted through panchayats with the assistance of non-governmental
organizations (NGOs).
Even
in the case of the organized flood forecasting service provided by CWC, there
is an immediate need to expand the system to include the States and rivers not
yet covered including the intra- State rivers. The observational network needs
to have fail-safe telemetry or fast communication channels to cut down the
transmission delays. The existing flood forecasting techniques and models need to be refined. A closer coordination
between different agencies will certainly upgrade the effectiveness of the
flood forecasting and warning system.
Flood warning work carried out in the
field by civil authorities such as the revenue officials, irrigation engineers,
public works engineers, and municipal bodies, involves informing the people in
time and executing rescue, relief and rehabilitation tasks. These arrangements
need regular review in association with the concerned sections of the people
and competent NGOs (non-government organizations).
7. THE CYCLONE
FORECASTING AND WARNING SYSTEM IN INDIA
Cyclone forecasing and warning services
are the responsibility of the India Metrological Department (IMD) which was in
fact established way back in 1875 in the aftermath of the severe cyclonic storm
of 1864 that devastated what was then the province of Bengal. One of the
primary objectives for setting up the Department was to issue warnings for
cyclones in the Bay of Bengal which disturbed the shipping activities to and
from Calcutta- the then capital of British India. It is also interesting to
note that the term “cyclone”, from the Greek word meaning the coils of snake,
was coined in India by Henry Piddington who, in a series of 23 Memoirs to the
Asiatic Society of Bengal in Calcutta, presented detailed account of the ocean
storms that occurred during 1839-1851. Thus
cyclone forecasting and warning services in India have a long and proud
record of over a century and have established a state- of-the art system that
is truly of world standard as we shall presently see.
Cyclone forecasting and warning involve
the following eight steps:
i)
Detection of a
weather system of the high seas that
shows signs of cyclone formation i.e., cyclogenesis.
ii)
Tracking the cyclone
once it forms.
iii)
Estimating the wind
force in the cyclone as it intensifies.
iv)
Anticipating its
future behaviour i.e. its probable track (speed and direction) and the place
and time of landfall on the coast.
v)
Sizing the eye of
the cyclone and interpolating the central pressure in the eye and the associated
winds especially at and after the landfall.
vi)
Estimating the
height, time and place of the storm surge.
vii)
Assessing the likely
rainfall as the cyclone moves overland and degenerates into a deep depression/
depression.
viii)
Formulation and
dissemination of forecasts and warnings at each significant stage and at
regular time intervals.
In order to accomplish the
abovementioned steps in the process of cyclone forecasting and warning, the
India Meteorological Department (IMD) utilizes the data from the following sources:
i)
Routine weather
observations from IMD’s own surface and upper air meteorological observations
network operating round the clock.
ii)
Weather reports from
about 280 merchant navy ships that constitute the Voluntary Observing Fleet.
iii)
Weather reports
(aireps) from commercial aircraft.
iv)
Radar reports from
IMD’s 10 high power cyclone detection radars on the coasts.
v)
Day and night cloud
imagery from INSAT geostationary satellite and the satellite derived data such
as the long-wave outgoing radiation and the cloud motion vectors (satellite
derived winds).
The meteorological data from the
network and from ships and aircraft are very important for synoptic analyses
and computation of parameters such as convergence, vorticity, and steering wind
field which enable an exhaustive scientific assessment of the energetic of the
cyclone and its prognosis including its likely track and the associated wind
and rain field. This exercise is done in a man-machine-mix mode in which the
skill of an experienced cyclone forecaster and the validated computer models
are made use of.
Cyclone detection radars and INSAT play
important roles in the cyclone forecasting and warning system as they keep the
cyclone under watch all the time and provide real time data instantaneously. While
radars probe the cyclone from the ground, the satellite provides the view from
the top.
IMD’s cyclone detection radar network
where each circle denotes the coverage of each radar which extends to 400 km
around the radar. It will be seen that there are 6 cyclone detection radars on
the east coast and 4 on the west coast. It may be recalled that the incidence
of cyclones is greater on the east coast as compared to the west coast.
There are two special features of IMD’s
powerful radar network. Firstly, its combined coverage is so dense that no
cyclone can come near the coast without being detected by one or more of these
radars. Secondly, the dense radar network is designed to provide an overlapping
surveillance in such a manner that even if one or two radars are not
operational at the crucial moment for any reason whatsoever ( a rare
occurrence, if at all), any cyclone will still be under the watch of one or
more radars. It is gratifying to note that this cyclone detection radar network
is to be gradually upgraded to a network of more versatile Doppler radars
within the next two years or so.
Once the current status of a cyclone
and its forecast behaviour are
available, the next step is to formulate the area-specific cyclone warnings
which are addressed to the concerned State Governments, Defence Services,
railways, Telecom agencies, airports, seaports, fisheries departments, special
users who have requested specific warnings and the general public (through the
electronic and print media). At the Central Government level, the Central
Relief Commissioner in the Ministry of Agriculture, Cabinet Secretariat and
Prime Minister’s Office are kept updated on the status of the cyclone.
Immediately on receipt of the first information regarding a cyclone, the Crisis
Management Committee, the Crisis Management Group and the Control Rooms get
energized at the Central level, the concerned State Government also initiating
similar action through the State Relief Commissioners.
IMD issues cyclone warnings in two
stages. In the first stage, a “CYCLONE ALERT” is issued about 48 hours before
the likely commencement of adverse weather on and along the coast. A “CYCLONE
WARNING” is issued about 24 hours before the likely landfall i.e., 24 hours
before the cyclone is expected to hit the coast. Of course, warnings to ports
and fisheries officials start much earlier as these are particularly
vulnerable. In fact, fishermen are warned not to venture out to the sea as soon
as a threat of cyclonic conditions is perceived in their area of
operation.
IMD
has developed mathematical models to make objective (Computer generated)
forecasts of cyclone tracks and the anticipated storm surge at the time of landfall. The cyclone warnings contain
information about the likely place and time of landfall and the height of the
associated storm surge.
It is not sufficient that the cyclone
warnings reach the State Governments at their headquarters and then the
warnings move to the local level through administration channels however quick
these might be. Time being of the essence in disaster management, cyclone
warnings should reach the target area simultaneously and preferably in the
local language. If the target area happens to cover more than one State, it is
advisable that the warnings are issued to each part of the area in the relevant
language. Issuing an omnibus multilingual message will be counterproductive.
Each warning should be succinct and in the required language. It should reach
each target area quickly and
simultaneously. This has been made possible through the Disaster Warning
Services (DWS) provided by INSAT.
The cyclone warnings originate from
IMD’s Area Cyclone Warning Centres (ACWCs) at Calcutta, Chennai and Mumbai with
the IMD Headquarters at New Delhi providing the guidance and coordination. The ACWCs are assisted by
three Cyclone warning Centres (CWCs) at Bhubaneshwar, Visakhapatnam and
Ahmedabad. It may be noted that the ACWCs and CWCs between them cover all the
cyclone prone States. The cyclone warnings for direct dissemination to the
desired target area are prepared in the appropriate language(s) and directly
broadcast from the concerned ACWC to the target area via the INSAT. In the
target area, a DWS receiving station needs only a dish antenna, receiver, and a
siren. Such sets are installed in selected villages, schools, panchayats,
revenue offices, police stations, and district offices. As DWS does not involve
any terrestrial wires, poles or cables, this communication system is also not
disturbed by cyclonic winds or heavy rains and the warning and de-warning
massages are disseminated without the threat of disruption. DWS is an
indigenous concept which has proved its worth during cyclone situations in the
past many years. There are already 250 DWS receiving stations in the field in
the cyclone prone States and further expansion is planned.
For warnings to seafarers, there is an
elaborate system of cyclone warning signals in the form of large visual
displays of different shapes (cylinder, diamond and other shapes) that are
prominently hoisted at seaports. These large signals of different shapes and
combinations- visible from a distance on the sea- denote different status of anticipated danger from
cyclonic weather or cyclone itself. These storm warning signals are of great
help to small boats and fishermen who do not have the type of fast
communication apparatus that large ships have.
It is worthy of note that IMD’s
responsibility in respect of cyclone forecasting and warning is for a region
larger than the Indian territory. By international arrangement under the aegis
of the World Meteorological Organization (WMO) which is a Specialized Agency of
the United Nations, IMD New Delhi is designated as the Regional Specialized
Meteorological Centre for Tropical Cyclones (RSMC- Tropical Cyclones). In this
capacity, it deals with all the cyclones that generate in the Bay of Bengal and
the Arabian Sea and issues “advisories” to neighbouring countries if their
territories are approached by a cyclone. There are only three such designated
centres in the northern hemisphere viz. RSMC-Tropical Cyclones at New Delhi
(India), RSMC- Typhoons at Tokyo (Japan), and RSMC- Hurricanes at Miami (USA).
In short, the cyclone forecasting and warning system in India is a proven
system recognized nationally and internationally.
Yet, the system can be made even more
effective. Apart form large scale expansion of the INSAT Disaster Warning
Service (DWS) by installing more DWS receiving stations in the field, a system
of aircraft reconnaissance flights will be very helpful. Such a cyclone probing
aircraft flight facility will be able to give the most reliable data on the
exact location of the eye (centre) of cyclone, the central pressure and the
wind field in the cyclone. These precise measurements will enable better
modelling of cyclone dynamics and thereby more accurate forecast of cyclone
track.