Polar Easterlies Definition

Understanding Polar Easterlies: Winds from the Poles

The Earth's atmosphere is a dynamic system, constantly in motion due to uneven heating from the sun. This movement creates various wind patterns, including the powerful jet streams and the gentler, yet significant, polar easterlies. Understanding these winds is crucial to grasping global weather patterns and climate dynamics. This article will demystify polar easterlies, explaining their formation, characteristics, and impact.

1. Defining Polar Easterlies: A Simple Explanation

Polar easterlies are cold, dry winds that blow from the east towards the west, predominantly in the polar regions (around 60° to 90° latitude) of both the Northern and Southern Hemispheres. Unlike the more powerful westerly winds at mid-latitudes, polar easterlies are relatively weak and inconsistent. Their existence is primarily a result of the pressure gradient between the polar high-pressure systems and the subpolar low-pressure systems. Imagine a slide: the high-pressure area is the top of the slide, and the low-pressure area is the bottom. The air, wanting to equalize pressure, slides down, creating the wind.

2. Formation and Dynamics: The Role of Pressure Gradients and the Coriolis Effect

The formation of polar easterlies is intricately linked to two key atmospheric forces:

Pressure Gradient Force: Cold, dense air sinks over the poles, creating high-pressure zones (polar highs). Conversely, relatively warmer air rises at the subpolar latitudes, forming low-pressure zones (subpolar lows). This pressure difference creates a force that pushes air from the high-pressure area towards the low-pressure area.

Coriolis Effect: As air moves from the poles towards the subpolar regions, the Earth's rotation deflects it. In the Northern Hemisphere, this deflection is to the right (eastward), and in the Southern Hemisphere, it's to the left (also eastward). This deflection, known as the Coriolis effect, is responsible for the easterly direction of these winds.

Without the Coriolis effect, the air would simply flow directly from the pole to the subpolar regions, creating a north-south wind. The Coriolis effect, however, significantly alters this, resulting in the characteristic east-west flow of the polar easterlies.

3. Characteristics of Polar Easterlies: Cold, Dry, and Weak

Polar easterlies are characterized by:

Low Temperature: Being situated over the icy polar regions, these winds carry extremely cold air masses.
Low Humidity: The air is generally dry, lacking substantial moisture content. This is because cold air holds less moisture than warm air.
Variable Speed and Consistency: Unlike the jet streams, polar easterlies are not consistently strong. Their speed varies significantly, often being weak and intermittent.
Seasonal Variations: The strength and extent of polar easterlies can fluctuate with the seasons. They are generally stronger during the winter months when the temperature difference between the poles and subpolar regions is more pronounced.

4. Impact on Global Weather and Climate: More Than Just Cold Winds

While seemingly insignificant compared to other wind systems, polar easterlies play a crucial role in:

Global Heat Distribution: Although weak, they contribute to the overall redistribution of heat from the poles toward the lower latitudes, though this contribution is minor compared to other atmospheric processes.
Sea Ice Formation and Movement: They influence the formation and movement of sea ice in polar regions, impacting ocean currents and marine ecosystems.
Weather Patterns at Higher Latitudes: They can influence weather patterns in polar and subpolar regions, contributing to occasional blizzards and other extreme weather events, especially when interacting with other weather systems.
Transport of Air Pollutants: Unfortunately, polar easterlies can also transport air pollutants and particulate matter over long distances, contributing to air quality issues in polar regions and impacting the delicate polar ecosystems.

5. Practical Examples: Observing the Effects

Imagine a weather map showing the movement of air masses. You'll likely observe the east-to-west movement of air masses in the high-latitude regions indicating the presence of polar easterlies. The extreme cold experienced in high-latitude regions during winter can be partially attributed to the influence of these winds, bringing frigid arctic air masses southward. The distribution of sea ice, observed through satellite imagery, is also partly influenced by the direction and strength of these winds.

Key Takeaways:

Polar easterlies are cold, dry winds blowing from east to west in polar regions.
Their formation is driven by pressure gradients and the Coriolis effect.
They are relatively weak and inconsistent, but still play a significant role in global climate and weather systems.
Understanding polar easterlies helps us comprehend global atmospheric circulation and its implications.

FAQs:

1. Are polar easterlies the same in both hemispheres? While they share the same general characteristics (cold, dry, easterly flow), their specific strength and patterns differ slightly between the Northern and Southern Hemispheres due to variations in landmass distribution and ocean currents.

2. How do polar easterlies compare to other wind systems? Compared to the strong westerly winds of mid-latitudes, polar easterlies are considerably weaker and less consistent. They are also much colder and drier.

3. Can polar easterlies cause extreme weather events? While not directly responsible for major storms, they can contribute to extreme cold events in subpolar regions and influence the movement of other weather systems, potentially exacerbating existing storms.

4. How are polar easterlies affected by climate change? Changes in the polar temperature gradient, caused by climate change, may alter the strength and behavior of polar easterlies, impacting weather patterns and sea ice distribution.

5. How are polar easterlies studied? Scientists use various tools and techniques to study polar easterlies, including weather satellites, weather balloons, and sophisticated climate models. These data sources allow them to monitor the winds’ speed, direction, and temperature, contributing to a greater understanding of their role in the Earth's climate system.

Search Results:

Polar easterlies | Article about polar easterlies by The Free … Find out information about polar easterlies. The rather shallow and diffuse body of easterly winds located poleward of the subpolar low-pressure belt; in the mean in the Northern Hemisphere, these... Explanation of polar easterlies.

Polar easterlies - (Earth Systems Science) - Vocab, Definition ... Polar easterlies are cold, dry winds that originate from the polar regions and blow from east to west. These winds are part of the Earth's atmospheric circulation and play a crucial role in influencing weather patterns and climate at high latitudes, contributing to …

Polar easterlies | meteorology | Britannica In the northern polar regions, where water and land are interspersed, the polar easterlies give way in summer to variable winds. …significant variations in these polar easterlies. In addition, the wind systems and the associated climate are seasonally dependent.

Polar easterlies - (Earth Science) - Vocab, Definition ... - Fiveable Polar easterlies are cold winds that blow from the polar high-pressure zones toward lower latitudes, predominantly from east to west. These winds are a significant component of the global wind system, influencing climate patterns and weather in polar regions and beyond.

polar easterlies - Glossary of Meteorology The rather shallow, irregular, and diffuse easterly winds located poleward of the subpolar low pressure belt. In the mean in the Northern Hemisphere, these easterlies exist to an appreciable extent only north of the Aleutian low and the Icelandic low. …

Global Winds: Definition, Patterns, Belts, and Causes - Science … 2 Feb 2023 · 3. Polar Easterlies. Location – 60° to 90° Latitude. They are dry, cold prevailing winds that blow from the high-pressure areas of the polar highs in both hemispheres. They flow towards low-pressure areas within the Westerlies at high latitudes.

Polar Easterlies - IASPOINT 21 Aug 2023 · Polar easterlies are an integral part of the global atmospheric circulation system and have a profound impact on our planet’s weather and climate. Polar easterlies are the cold, dry winds that flow from the polar regions (both North and South Poles) towards the middle latitudes.

Marine Glossary - Starpath polar easterlies A prevailing east wind above the arctic and antarctic circles, shown schematically in G216. The "polar easterlies" are a natural part of the global circulation. Air heats and rises at the equator and moves north aloft. At the pole it is cold and descends.

Polar Winds - Kids Earth Science The winds are therefore called Polar Easterlies. Scientists describe and name winds based on the direction from which they are blowing. Oceanographers do the opposite. Scientists studying ocean currents describe currents based on the direction they are …

The Polar Winds or the Polar Easterlies - Physical Geography 30 Nov 2020 · They are also called the polar easterlies, from the direction in which they blow. This belt of low pressure is more persistent in the summer season and generally disappears in the winter season. However, the Icelandic and Aleutian …

Polar easterlies - (Intro to Climate Science) - Vocab, Definition ... Polar easterlies are cold winds that blow from the east toward the west near the poles, particularly in the Arctic and Antarctic regions. These winds are a crucial component of the global atmospheric circulation patterns, forming as a result of high-pressure areas at the poles where cold air sinks and moves outward, influencing weather patterns ...

Polar Easterlies - Geography Notes - Prepp Polar easterlies are the dry, cold prevailing winds that blow around the high-pressure systems of the polar highs at the North Poles and the South Poles. When chilly air flows from the poles to the equator, a wind pattern like this emerges.

What are the polar easterlies? | Weather | wfmz.com 28 Jul 2011 · The polar easterlies are the dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards low-pressure areas within the...

Polar easterlies - Academic Dictionaries and Encyclopedias The polar easterlies are the dry, cold prevailing winds that blow from the high pressure areas of the polar highs at the north and south poles towards the low pressure areas of the polar fronts between 60 and 90 degrees north and south.

Polar easterlies - Wikipedia The polar easterlies are one of the five primary wind zones, known as wind belts, that make up our atmosphere's circulatory system. This particular belt of wind begins at approximately 60 degrees north and south latitude and reaches to the poles.

polar easterlies - English definition, grammar, pronunciation, … The polar easterlies (also known as Polar Hadley cells) are the dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the North and South Poles towards the low-pressure areas within the westerlies at high latitudes.

Planetary Winds: Easterlies and Westerlies - Mapping Around Polar Easterlies. Polar easterlies are prevailing winds that blow from the polar high-pressure areas (near the poles) towards the subpolar low-pressure belts at around 60-65 degrees latitude in both hemispheres. In the Northern Hemisphere, they blow from northeast to southwest, and in the Southern Hemisphere, they blow from southeast to northwest.

What are the polar easterlies? | News | wfmz.com 4 Apr 2010 · The polar easterlies are the dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards low-pressure areas within the...

Where Are the Polar Easterlies Located? - travelasker.com 27 Jan 2024 · The polar easterlies are prevailing winds that blow from the polar regions towards the mid-latitudes. These winds are part of the global circulation pattern known as the Hadley cell, which is responsible for the movement of heat and moisture in the Earth’s atmosphere.

What does Polar easterlies mean? - Definitions.net The polar easterlies are the dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards low-pressure areas within the Westerlies at high latitudes.