The main reason behind the months of preciptation in the graphs of monsoon climatic regions being different is:
Answers
Tropical Monsoon Climate
The tropical monsoon climate experiences superabundant precipitation like that of the tropical rain forest climate, however it's focused within the high-sun season. Being settled close to the equator, the tropical monsoon climate experiences heat temperatures throughout the year.
Geographical Distribution
The monsoon climate is found on the coastal regions of southwest Asian nation, Sri Lanka, Bangladesh, Myanmar, Southwestern continent, French geographic area, and northeast and southeastern Brazil.
Controlling Factors
The major dominant issue over the monsoon climate is its relationship to the monsoon circulation. Recall that the monsoon could be a seasonal amendment in wind direction. The "classic" monsoon circulation of Asia exhibits associate onshore flow of air (air moving from ocean towards land) throughout the summer or high-sun season, and offshore air flow (air moving from land toward water) throughout the winter or low-sun season. The amendment in direction is because of the distinction within the means water and land heat.
Changing pressure patterns that have an effect on the seasonality of precipitation conjointly occur in continent. throughout the high-sun season, the ITCZ induces rain whereas the semitropical high creates dry conditions. The monsoon climate of continent, and South America for that matter, are generally settled on tradewind coasts.
Precipitation
Seasonality of its precipitation is that the hallmark and most well-known characteristic of the monsoon climate. several assume that the term "monsoon" suggests that wet weather, once in truth it describes associate atmospherical circulation pattern. although the annual quantity of precipitation is sort of kind of like that of the rain forest, monsoon precipitation is focused into the high-sun season.
Maritime equatorial and maritime tropical air lots travel from the ocean on to land throughout the summer, wherever they're elated by either convection or convergence of air to induce condensation. Locally, orographic uplift is a very important mechanism for promoting precipitation. As air travels into the Indian landmass, it's elated by the range of mountains, inflicting cloud development and precipitation.
The low-sun season is characterised by a brief drought season once air mass inhibits precipitation formation. within the case of the Asian monsoon, the replacement of the thermal low with the subsidence of the Siberian High suppresses uplift. Air lots that dominate this era are dry given their continental origin (cT, cP) or stability (mTs).