STORY OF CYCLONES

 

STORY OF CYCLONES

 

 Nikunja Bihari Sahu

     

         Generally, October has been the month of major atmospheric disturbances over the Bay of Bengal.  This is the month when ravaging cyclones used to form in the far seas and race miles across the waters with awesome speed to unfold on the eastern Indian coast. While the Phailin struck Orissa on October 12, 2013, exactly a year later the Hudhud pounded the coastal districts of Andhra Pradesh. This was followed by Titli that battered both the Odisha and Andhra coast recently with heavy rain and gale winds. All these cyclones left behind a trail of destruction by flattening thousands of mud and thatched houses and tearing down road and communication links. But people are still unaware of the impacts of the cyclone as evident from their reluctance to leave their ancestral homes for relocation to safer places.  Hence, an understanding of cyclones is essential. 

Origin and Development

               Given the vast devastation as described above, the huge strength of the Cyclone can be easily understood. The secret to its enormous prowess lies on a very basic property of Water. Water, unlike all other liquids, has a high Latent Heat of Vaporization which is essentially the heat released when Water in gaseous state changes its form to liquid state as a result of Condensation. This value for Water is 2.5 x 106 J/kg in contrast to other liquids like Ammonia: 1.2 x 106 J/kg, Propane: 4.2 x 105 J/kg, Ether: 3.9 x 105 J/kg, Carbon Tetrachloride:   2.2 x 105 J/kg.

          A Cyclone has its humble beginning as a small twister over the far tropical seas as the sunrays heat up water surface producing copious mass of warm and moist air. Sometimes, the moist air mass lays stationary as a huge cloud over the sea surface without dispersing away. This mass is highly unstable in nature that eventually becomes the cradle for the Cyclone. Further heating causes streams of air rising up within the moist air cloud creating a low pressure region. Surrounding mass of moist air rushes towards the region that curves around due to the Earth’s spin. On reaching the Low pressure centre, the mass of moist air rises upward and expands suddenly at the higher atmosphere eventually getting cooled. The cooling triggers condensation of millions of water vapours present in the moist air releasing a large quantity of heat to the surrounding due to the high Latent heat of Water. The heat that was released evaporates more amount of moist air from the sea surface that further feeds and fuels the cyclic process and keeps it raging for weeks. Under favourable conditions, the situation rapidly intensifies into a sequence of events such as Depression, Deep Depression, Cyclonic storm and Severe and Very Severe Cyclonic Storms with wind speeds reaching as high as 300 km/h.

        Although the common name for such typical storms is Hurricanes, these are named differently in different local regions such as Typhoons in the Pacific and Cyclones in the Bay of Bengal. The word Cyclone is actually a Greek word that means coil of a Snake which was first used by a British meteorologist to refer to small depressions created over the Bay of Bengal.

             Eventually, the storm of the far seas heads towards the land and appears as killer winds for the coastal population. But on reaching the land, it quickly subsides as no moist air is available to keep its cyclic process going. Before that, it had wrecked widespread damage to life and property.

 Damage and Destruction

            Of the 23 cyclones in the last 300 years that have each resulted in loss of more than 10,000 lives, 20 have been formed over the Bay of Bengal and affected India. Almost 75% of the cyclones that have killed more than 5,000 people during this time have been originated in this region. This, despite the fact that only 7% of the World’s cyclones in a year are generated in this part of the globe and also the fact that cyclones in the Bay of Bengal and the Arabian Sea are of moderate intensity as compared to the hurricanes raged in the Western Atlantic and Typhoons in the Western Pacific regions.  The Super cyclone of October 29, 1999 killed around 10,000 people in Odisha. One reason for the heavy casualty in the past is that the Indian coastline is densely populated.

   Weather Forecasting Has Come of Age

          But the situation has been drastically changed over the years owing to very accurate weather forecasting as evident from the lesser death tolls of Phailin (38), Hudhud (nearly 100) and Titli (62). Weather forecasting today has come of age and the science has developed considerably enabling very accurate and reliable prediction of cyclones facilitating relief and rescue operations. With the advent of the Space Age, it has now become possible to directly see the cyclone with satellites and monitor its progress in real time by satellite imagery allowing an early warning to be issued for befitting response from the Govt. and the people. This can be appreciated from the fact that while an early warning for the Super cyclone of 1999 could be generated only 2 days earlier , the same for Phailin was issued 4 days beforehand allowing sufficient time for the Govt.  to mobilize its resources  to carry out one of the biggest  evacuation drives in Indian history . 

  Preparedness is Safety

           Like many other natural calamities, a Cyclone cannot be prevented with the present day technology. But timely warning of the impending disaster with accurate meteorological inputs can bolster the preparedness of the people to lessen the scale of devastation. The prime responsibility of the Govt. in the post Cyclonic period is to restore power, road and communication links.  As the cyclone abruptly  releases vast amount of water on land collected from the seas in its huge mass of moist air (often half the size of India), a flash  flood situation in the aftermath of the cyclone is very likely and the Govt. must be prepared to face that. Finally, we must go by the weather reports meticulously to keep ourselves prepared for ensuring individual and collective safety. 

                                                

 


                                                Education Officer

                                                Dhenkanal Science Centre

                                               (National Council of Science Museums

                                                   Ministry of Culture, Govt. of India)

                                                 (Near Rajbati)

                                                  Dhenkanal-759001

                                                    Phone: 8018708858

                                                ODISHA

 

 

 

 

Further Reading :

 

1.     Conquest of Phailin by Nikunja Bihari Sahu (Science Horizon: Feb, 2014     issue).

 

2.     Hunt of the Hudhud by Nikunja Bihari Sahu (Science Horizon: June, 2015  issue).

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

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