Wednesday, April 11, 2012

Climate and Typhoons in Beppu, Oita, Kyushu

Oita, along with most of the island of Kyushu, hosts a humid subtropical climate classified as Cfa in the Koeppen Classification system. 



















A lack of any dry season in combination with hot summers defines a Cfa climate. In Beppu, Oita, this type of climate allows for plentiful rain in the summer months while maintaining temperatures in the higher 80s (degrees Fahrenheit). The precipitation levels drop during the winter months along with the temperatures, but a measurable amount of moisture remains. 





Originating in the tropical Pacific Ocean, the Maritime Tropical (mT) air mass located just south of Kyushu around the subtropical high (STH) contributes to Cfa climate. In the summer months when the warmer isotherms, or lines connecting the same air temperatures rest up north because of the jet stream positioning, this air mass moves toward Kyushu (Ritter). Created in a stable STH, mT air masses are “warm, moist, and usually unstable” leading to precipitation and the warm temperatures (“Air Masses”). When the jet streams move the isotherms south for the winter, the maritime polar (mT) air mass just north of Japan brings with it cool and moist air keeping precipitation in the area year-round.


Purple indicates mT
Yellow indicates mP
Along with jet streams and air masses, low-pressure systems with organized convection and cyclonic movement, also know as typhoons or hurricanes, commonly affect Kyushu (Landsea). The typhoon season begins around May and peak season occurs in August and September (“Typhoons”). The main islands of Japan, especially Kyushu and Shikoku, usually experience three typhoons a year making preparation and clean-up of the aftermath normal for the population (“Typhoons”). 




Typhoon moving toward the main islands of Japan

During Typhoon in Tokyo

Clean-up after Typhoon Talas
A typhoon moving right over Kyushu





Sources:

Landsea, Chris. “FAQ.” Atlantic Oceanographic and Meteorological Laboratory. http://www.aoml.noaa.gov/hrd/tcfaq/A1.html

Ritter, Michael. “Air Temperature and Air Mass Movement.” http://www4.uwsp.edu/geo/faculty/ritter/geog101/textbook/temperature/temperature_air_masses.html.

“Typhoons.” http://www.japan-guide.com/e/e2117.html



Sources of Illustrations (In order of appearance):
Ibid.
Ibid.
http://sakura-hotel-ikebukuro.com/blog/2011/09/post_46.php
http://www.eorc.jaxa.jp/en/imgdata/topics/2011/tp111101.html

1 comment:

  1. What's up Jane, I am Joe Gonzales, and I have been reading your most recent post. I must say this is an excellent post, packed with well explained concepts. The content describes the climate type, air masses, and typhoon storm patterns for the region, all of which are accurate and precise. I found your explanation of air masses to be particularly interesting as well as how you showed the relationship between air masses and typhoons. You also stated that typhoons strike this region three times a year on average, how many casualties and costs in damages are there typically per year as a result? Just a thought, however, great post! Good job!

    ReplyDelete