There are three main types of winds that affect the climate of Tokyo. The westerlies blow from the west, the trade winds from the northeast, and the southern hemisphere currents blow from the southeast. The two major types of winds have distinct characteristics. The summers in Tokyo are muggy, with high temperatures, and the winters are dry and mild. Here are some interesting facts about the climate of Tokyo.
Temperatures in Tokyo are mostly temperate. They usually remain around 30 degrees C. There is one record high of 39.5 degrees Celsius in Tokyo on July 21, but researchers disagree about what caused the extreme temperatures. The first southerly wind of the year is known as “haru ichiban,” and it marks the arrival of warm spring. But the heat wave can also bring heavy snowfall, and avalanches can occur.
The winters are very mild, with cool temperatures. In summer, high-pressure air masses from China enter the Sea of Japan, bringing strong southerly winds that travel northward toward the low-pressure zone of the Pacific Ocean. These powerful winds bring warm, moist air to Japan, making it a hot, humid place to live. However, they can cause avalanches and large fires, so the winters are typically very cold.
The “mean daily maximum” and “mean daily minimum” graphs in Tokyo show days when certain levels of precipitation occur. Although monsoon climates are often underrepresented, tropical and subtropical climates tend to underestimate precipitation amounts. The “mean daily maximum” and the “cold nights” graphs can help you plan your vacation. You can also choose your preferred units of wind speed, such as km/h.
The daily high and low temperatures in Tokyo vary. The temperature in winter is the coldest. In summer, the high and low seasons are similar. The rainy season ends when the “baiu zensen” is pushed northward. The two seasons are the same in summer. The winter is cooler and the rainy season lasts until late May. In the summer, the weather in Japan is quite mild.
The monthly precipitation and wind speed diagrams in Tokyo are useful for vacation planning. The temperatures of the different seasons are displayed, and the monthly rainfall and wind speeds are displayed. The rainy season in Tokyo is a little warmer than in the rest of Japan. It is also colder than the rest of Asia, but it can still be hot in some areas. The temperatures in Japan are influenced by several factors.
The rainy season in Tokyo is triggered by the presence of low-pressure air masses from the Pacific Ocean. The result is the rainy season. While the monsoon wind brings rain to the city, the baiu zensen is pushed northward. The summer months are hot, and the baiu zensen is the strongest of all. Aside from the seasonal winds, high-pressure air masses are dominated by high-pressure air masses.
In Tokyo, the weather is influenced by the winds and weather conditions. The weather in Tokyo is humid subtropical with warm, humid summers and mild winters. The most common wind in Japan is the northwesterly wind from Siberia. The cold air mass brings cold air to Japan, resulting in heavy snowfall on the Sea of Jemisin. The southwesterly wind brings sunny weather to the Pacific side.
The rainfall and wind speed in Tokyo are similar. The rainy season ends in October, while the rainy season lasts until April. The “baiu zensen” is pushed northward, bringing warm moist air to the country. This air mass is responsible for the hot summers in Japan. So, the wind patterns in the city are important. The humidity and heat is influenced by the amount of precipitation.
There are two main types of global winds in Tokyo. The south-westerly wind carries cold air from Siberia to Japan. The north-easterly wind carries warm air from the Pacific to the Sea of Japan. During the summer, the northwesterly wind is the opposite. In winter, the northwesterly wind carries cold air from Siberian regions to the mainland of Japan.