Chapter 16: Problem 25
Infer Why don't hurricanes form in Earth's polar regions?
Short Answer
Expert verified
Hurricanes don't form in polar regions due to cold ocean temperatures and unfavorable atmospheric conditions.
Step by step solution
01
Understand Hurricane Formation
Hurricanes form over warm ocean waters, typically when the sea surface temperature is at least 26.5 degrees Celsius (about 80 degrees Fahrenheit). These warm waters provide the heat and moisture that power the storm.
02
Identify Polar Ocean Temperatures
Polar regions are known for their cold climates. The ocean temperatures in polar areas are significantly lower than the 26.5 degrees Celsius threshold required for hurricane formation, often hovering at or below freezing.
03
Examine Atmospheric Conditions
Hurricanes require not only warm ocean water but also specific atmospheric conditions, such as moisture in the mid-troposphere, minimal vertical wind shear, and a sufficiently large Coriolis force, which is weak at the poles. These conditions are not present in polar regions.
04
Conclude Why Hurricanes Don't Form
Given that polar regions lack both the warm ocean temperatures and the favorable atmospheric conditions necessary for hurricane formation, hurricanes cannot develop in these areas.
Unlock Step-by-Step Solutions & Ace Your Exams!
-
Full Textbook Solutions
Get detailed explanations and key concepts
-
Unlimited Al creation
Al flashcards, explanations, exams and more...
-
Ads-free access
To over 500 millions flashcards
-
Money-back guarantee
We refund you if you fail your exam.
Over 30 million students worldwide already upgrade their learning with Vaia!
Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Ocean Temperature
The temperature of the ocean is a crucial factor in the formation of hurricanes. For a hurricane to form, the ocean surface temperature must be at least 26.5 degrees Celsius (or about 80 degrees Fahrenheit). This warmth is essential because it provides the heat and moisture that fuel these intense storms.
However, in polar regions, ocean temperatures are much colder and often remain at or below freezing. This means that in these icy areas, the waters cannot reach the necessary warmth to support hurricane development.
This cold environment prevents the formation of hurricanes, as there is insufficient thermal energy to initiate or sustain such powerful weather systems.
However, in polar regions, ocean temperatures are much colder and often remain at or below freezing. This means that in these icy areas, the waters cannot reach the necessary warmth to support hurricane development.
This cold environment prevents the formation of hurricanes, as there is insufficient thermal energy to initiate or sustain such powerful weather systems.
Atmospheric Conditions
In addition to warm ocean temperatures, specific atmospheric conditions are needed for hurricanes to form. One key factor is the presence of moisture in the mid-troposphere, the layer of the atmosphere where weather largely occurs. Without adequate moisture, storms cannot gather strength and sustain themselves.
- Moisture: Mid-atmospheric moisture acts as fuel for storms, helping them grow and intensify.
- Vertical Wind Shear: Minimizing differences in wind speed and direction at various altitudes, known as vertical wind shear, is essential. Too much wind shear can disrupt storm formation.
- Coriolis Force: A substantial Coriolis force is necessary to initiate the rotation of storms, aiding in their spiral structure.
Coriolis Force
The Coriolis force is one of the drivers behind what makes a hurricane spin. It results from Earth's rotation and causes moving air to swirl, an effect that strengthens with distance from the equator. This force is crucial for giving hurricanes their characteristic circular movement.
At the poles, the Coriolis force is notably weaker because there is little rotational influence compared to the mid-latitudes. Without enough of this force, hurricane-like storms cannot form or maintain their circular, spiraling structure, which is why hurricanes are not typically seen near the poles.
In regions closer to the equator, the Coriolis effect is strong enough to influence storm systems, allowing for the development of hurricanes with a distinct rotational pattern.
At the poles, the Coriolis force is notably weaker because there is little rotational influence compared to the mid-latitudes. Without enough of this force, hurricane-like storms cannot form or maintain their circular, spiraling structure, which is why hurricanes are not typically seen near the poles.
In regions closer to the equator, the Coriolis effect is strong enough to influence storm systems, allowing for the development of hurricanes with a distinct rotational pattern.
Polar Regions
Polar regions are characterized by extremely cold temperatures and ice-covered landscapes. These areas remain inhospitable to hurricane formation due to several key factors.
Firstly, the consistently low ocean and atmospheric temperatures do not allow the thermodynamic conditions necessary for these storms. Secondly, the atmospheric composition lacks the necessary moisture and is often too variable and unstable due to the harsh polar conditions.
Firstly, the consistently low ocean and atmospheric temperatures do not allow the thermodynamic conditions necessary for these storms. Secondly, the atmospheric composition lacks the necessary moisture and is often too variable and unstable due to the harsh polar conditions.
- Low Temperatures: The icy environment does not allow sea surface temperatures to rise to hurricane-supporting levels.
- Atmospheric Instability: The polar atmosphere's conditions do not favor stable storm development.