Sunday, June 06, 2010

Cyclone History for Karachi

Let not the cyclone haunt us. Better scare it away. Away from our minds. But we still have to be mindful of the facts about cyclones. The facts however, remain that each year before the onset of monsoon (15 April to 15 July) and also after its withdrawal (15th September to 15 December), there is always a distinct possibility of the cyclone storm to develop in the north Arabian Sea.
          The word “cyclone” is of Greek origin and means a “coil of snake”. No doubt, fully developed cyclone not only resemble the coil of the snake they have the venom of thousands of snakes as far as there killing capability is concerned. These giants kill in three ways-by coursing heavy to very heavy continues down pour leading to floods strong to very strong sustained winds, and tidal waves. The distinguishing property of the cyclonic storm is, however, the onslaught of tidal waves with often a company the storms along with strong sustained winds and torrential rain.
          Tropical cyclone are classified according to the maximum winds which a company them as indicated in the following.
          Depression – winds up to 33 Knots, Cyclonic Storm – winds from 34 to 47 Knots, Severe Tropical Strom – Winds from 48 to 63 Knots, Hurricane – winds of 64 Knots or more.
          The major killing factor is there for the tidal wave assisted by very strong winds as regards tidal waves possible coincidence of the time of passage of an expected cyclonic storm with high and low tide times and loner dates can appreciably add her decrees the actual heights of the tidal waves.
          This important factor is, therefore, given due consideration when forecasting the passage of the cyclonic storm into the costal areas.
          It is worthwhile to evaluate how great is the danger of cyclonic storm striking Karachi or other costal areas of Pakistan. Because of its very high population and industrial growth, Karachi merits special attentions. Although nobody except providence knows what fate awaits us, the changing natural processes and events do provide a clue to us. One of the parameter utilized by Meteorologist is the climatology or past records of weather events.
In this connection meteorological data about the cyclonic storms in the north Arabian sea is available for more then a century. During the last 100 years a number of cyclonic storms have struck Pakistan’s costal areas.
           The years involved were 1895, 1902, 1907, 1948, 1964 and 1985.
           The cyclonic storm in 1964 which actually enter the Indian coast did cause the great loss of life and property in Hyderabad and Tharparkar districts as it moved north east ward into south eastern areas of Sindh. It is strange that three cyclonic storms – two in the year 1902 (13th May & 16th June) and one in 1907 (6th June) stuck the coast in the vicinity of Karachi during a short span of six year? The other two cyclonic storms in the years 1895 and 1984 struck the Mehran cost near Pasni and Jiwani respectively.
            The cyclonic storm in 1985 which moved was Karachi actually had weakened over the sea while still a few 100 Kilometers away south of Karachi. It did, however, cause concern and panic for Karachiites.         
          
            Cyclone Gonu 2007 , Super Cyclonic Storm Gonu is the strongest tropical cyclone on record in the Arabian Seaand is also the strongest named cyclone in the northern Indian Ocean. The second named tropical cyclone of the 2007 North Indian Ocean cyclone season, Gonu developed from a persistent area of convection in the eastern Arabian Sea on June 1. With a favorable upper-level environment and warm sea surface temperatures, it rapidly intensified to attain peak winds of 240 km/h (150 mph) on June 3. Gonu weakened after encountering dry air and cooler waters and early on June 6, it madelandfall on the eastern-most tip of Oman, becoming the strongest tropical cyclone to hit the Arabian Peninsula. It then turned northward into the Gulf of Oman, and dissipated on June 7 after making landfall in southern Iran.

The Yemyin 2007
On October 19  an area of low pressure which located to the south east of SalalahOman had intensified in to a tropical depression and was assigned the number ARB 02. On October 21  the system intensify into a Deep Depression while it lay 700 km south of SalalahOman, near the east coast of Somalia. It lost its strength while crossing the Gulf of Aden due to entry of dry air and land interaction as it passed close to the northeastern coast of Somalia. It later was downgraded to a Depression, named TC 03A by the JTWC. On October 24 it made landfall on the south-eastern coast of Yemen, and caused severe flooding, causing loss of 180 lives.
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