tropical monsoon climate
Natural Topography: Location and Characteristics of Main Landforms, The hot and dry pre-monsoon season, from March to May, The rainy monsoon season, from June to October. It refers to many elements including temperature, precipitation, humidity, air pressure, wind movement, and direction. Depression is a region of low atmospheric pressure. These storm clouds are usually 5 km wide and 8 km high. Astronomical tides in combination with cyclonic surges lead to higher water levels and hence severe flooding. Let’s find more characteristics of a tropical monsoon climate. Average temperatures in January vary from about 17˚C in the northwestern and northeastern parts of 20˚-21˚C in the coastal areas. This difference in pressure causes the winds to flow from the high-pressure area to the low-pressure area that is, from the ocean to the land area. These climates are found primarily in southern and southeastern Asia and have the combined abbreviation Am…. This site uses Akismet to reduce spam. This is because of: Most of the damage caused by the cyclones occur in the coastal regions of Khulna, Patuakhali, Barisal, Noakhali and Chittagong and the offshore island of Bhola, Hatiya, Sandwip, Mapura, Kutubdia, Maheshkhali, Nijhum Dwip, Urir Char and other newly formed islands. Required fields are marked *. There is little that can withstand a great mass of onrushing water often as high as 6m. ( Log Out /  The average annual rainfall in Bangladesh varies from 1500 mm in the west-central part to over 3000 mm in the northeast and southeast. since the wind in this season blows forms the land to the ocean, almost dry conditions prevail and very little rainfall occurs at this time. LOCATION The monsoon climate beyond the equatorial region between 10 and 25 and North… Widespread cloud cover lowers the temperature during the later of the pre-monsoon season. warmer than rest storm area, more violent storm, eye. Name two high-risk areas to be hit by cyclones. It has a tropical climate because of its physical location. Higher rainfall in the northeast is caused by the additional effect of the orographic uplifting provide by the Meghalaya plateau. The center of the cyclone is calm and is known as the eye. Yes, i agree this is really useful content, Your email address will not be published. The average temperature in January varies from 17˚C in the northwest and northeast of the country to 20˚C-21˚C in the coastal areas. The rain in this period is caused by conventional storms (thunderstorm) or nor-westers (locally called a Kal Baiskhkhi). it is not that usefull and not enough detailed in some parts and so much detailed in some other parts, This syllabus according to Bruneian O level Geography Paper. Cyclones develop over warm seas when the surface temperature is more than 27˚C. Bangladesh extends from 20˚34΄N to 26˚38΄N latitude and from 88˚01΄E to 92˚41΄E longitude. Seasonal changes of this wing direction are caused by the differential heating and caused by the differential heating and cooling of landmass and oceans between summer and winter. The monsoon wind blows from the northeast (towards the sea) in winter (the dry monsoon) and from the southwest (towards the land) in summer (the wet monsoon). The Bengal calendar year is traditionally divided into six seasons: Each season lasts on average two months, but some seasons merge into other seasons, while others are short. At times more than two to three weeks of rainfall may occur in Sylhet and Cox’s Bazar areas. Again, higher rainfall in the northeast is caused by the additional optional uplifting effect of the Meghalaya plateau. The amount of rainfall during the is season varies from 1000 mm in the west-central part of the country to over 2000 mm in the south and northeast. On average, five severe cyclonic storms hit Bangladesh every year and the accompanying surge can reach as far as 700 km inland. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. Technically, a cyclone is an area of low pressure where strong winds blow around a center in an anticlockwise direction in the Northern Hemisphere and a clockwise direction in the Southern Hemisphere. The minimum temperature in the extreme northwest in late December and early January can be as low as 3˚C to 4˚C. winds are a very light eye, usually not 25 30/hr rain practically absent, contrast, strongest heaviest occur just outside this central eye. However, the cold winter air that moves into the country from the northwestern part of India loses much of its intensity by the time it reaches the northwestern corner of the country.

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