HK climatology Flashcards
Climate zone
Subtropical
summer monsoon
In summer, the air over the Asian land mass heats up faster than that over the ocean. This creates a pressure difference and brings a southwest wind from the ocean towards the land.
Winter monsoon
The air over the Asian land mass cools down faster than that over the ocean. The resulting pressure difference brings a northeast monsoon from the land towards the ocean.
Tropical cyclone
a rapidly rotating storm system characterized by a low-pressure center
western North Pacific: typhoon
North Atlantic: hurricane
North Indian Ocean: cyclone
Tropical Cyclone Classification
Tropical Depression (TD) <63 km/hr Tropical Storm (TS) 63-87 Severe Tropical Storm (STS) 88-117 Typhoon (T) 118-149 Severe Typhoon (ST)* 150-184 Super Typhoon (SuperT)*185 or above
How does a typhoon form
The process begins when the surface of the ocean heats up. Air from surrounding areas with higher air pressure pushes in to the low pressure area.
The wind begins to spiral (counterclockwise) toward a center of low pressure, drawing moisture to the center, which forms the eye. When the storm becomes organized, it develops into a tropical depression. Once wind speeds reach 39 miles per hour, it becomes a tropical storm.The eye of low pressure develops, and the storm begins to rotate and gain in strength. The storm becomes a typhoon when it reaches wind speeds of 74 miles per hour.
Requirements for tropical cyclone
- sufficiently warm sea surface temperatures (26.5C)
- atmospheric instability,
- high humidity in the lower to middle levels of the troposphere,
- enough Coriolis force to develop a low pressure center by spiralling (can’t be too close to equator)
- a pre-existing low level focus or disturbance,
- low vertical wind shear.
Where are most of the typhoons formed
Northwest Pacific Ocean