Fronts are not associated with tropical systems.
A stationary front typically precedes a mid-latitude cyclone. This front forms when a cold front and a warm front meet and stall, creating an area of temperature gradient that can lead to the development of a cyclone.
In the first stage of a wave cyclone, an initial warm front forms. This front is created as warm air is forced up and over a retreating colder air mass, leading to the development of clouds and precipitation.
An occluded front is the type of front that is only associated with a mature mid-latitude cyclone. It forms when the cold front of a cyclone catches up to the warm front, lifting the warm air mass above the cooler air mass, creating a mix of both cold and warm characteristics.
Mid-latitude cyclones typically produce both a cold front and a warm front. These will usually merge to form an occluded front.
The correct designation for a hurricane is a tropical cyclone. It can also be referred to as a typhoon or cyclone, depending on the region where it forms.
stationary front
A storm system called a 'Tropical Cyclone' also known as a 'Hurricane' if it forms over the Atlantic, a 'Cyclone' if it forms over the Indian ocean and a 'Typhoon' if it forms over the Pacific.
A hurricane that forms over the Indian ocean is called a cyclone.
The front that forms when a warm air mass is trapped between cold air masses and is forced to rise is called a occluded front. This occurs in the process of cyclone development, where a cold front catches up to a warm front, lifting the warm air off the ground. As the warm air rises, it can lead to cloud formation and precipitation.
Because the Water is simply not Warm enough to produce one. Its called a tropical cyclone because a Cyclone forms over warmer waters... in the tropics
a wave cyclone accompanying the cold front
The term for when a bend forms in a cold front and creates an area of low pressure with rotating winds moving toward the central low pressure region is called cyclogenesis, specifically when it leads to the development of a mid-latitude cyclone or extratropical cyclone. This process involves the intensification of the low-pressure system as warm and cold air masses interact along the front.