3. Tropical Storm in LEDC Cyclone One Bravo – Bangladesh · Severe tropical cyclone with winds up to 250 kph recorded · Formed over Bay of Bengal in the Indian Ocean in May 1997 · Struck land at Chittagong on the south-eastern coast of Bangladesh · 111 deaths · 500,000 people left homeless · Wells contaminated by salt water · 1 million people had no fresh water · Many outbreaks of diarrhoea · Cash crops and 2000 cattle lost
4. What is a Monsoon? Even in the tropics, where the weather is warm year round, the march of the seasons has a profound influence on the rhythm of life. Rainy seasons, usually referred to as monsoons , alternate with dry seasons and each has its own distinct pattern of prevailing winds. The term “monsoon” is derived from the Arabic word “mausim” which means season. Ancient traders sailing the Indian Ocean and Arabian Sea used it to describe a system of alternating winds that blow persistently from the northeast during the winter and from the opposite direction, the southwest, during the summer. It is now well understood that seasonal reversals of wind direction occur because of temperature differences between the land and sea across all of the Tropics. There are many features in common to these summer monsoon circulations, but the most recognizable are the seasonal changes in rainfall patterns, both increases and decreases.
5. Cyclones Tropical storms are intensive low pressure weather systems and can often be referred to as Hurricanes, Cyclones, Typhoons or Willy willies. There source regions are in major oceans between the tropics of Cancer and Capricorn. They require a sea temperature over 27 degrees centigrade in order to form. However they only occur for a few months in the summer when the sea temperatures are at their highest . They move mainly northerly and/or westerly. They bring strong winds and high rainfall as well as storm surges.