The Northern Hemisphere of Earth is the half that is north of the equator. For other planets in the Solar System, north is defined as being in the same celestial hemisphere relative to the invariable plane of the solar system as Earth's North pole.
Due to the Earth's axial tilt, winter in the Northern Hemisphere lasts from the winter solstice (typically December 21 UTC) to the March Equinox (typically March 20 UTC), while summer lasts from the summer solstice (typically June 21 UTC) through to the autumnal equinox (typically September 23 UTC). The dates vary each year due to the difference between the calendar year and the astronomical year.
Geography and climate
The Arctic is the region north of the Arctic Circle. Its climate is characterized by cold winters and cool summers. Precipitation mostly comes in the form of snow. The Arctic experiences some days in summer when the Sun never sets, and some days during the winter when it never rises. The duration of these phases varies from one day for locations right on the Arctic Circle to several months near the North Pole, which is the middle of the Northern Hemisphere.
Between the Arctic Circle and the Tropic of Cancer lies the Northern Temperate Zone. The changes in these regions between summer and winter are generally mild, rather than extreme hot or cold. However, a temperate climate can have very unpredictable weather.
Tropical regions (between the Tropic of Cancer and the equator) are generally hot all year round and tend to experience a rainy season during the summer months, and a dry season during the winter months.
In the Northern Hemisphere, objects moving across or above the surface of the Earth tend to turn to the right because of the coriolis effect. As a result, large-scale horizontal flows of air or water tend to form clockwise-turning gyres. These are best seen in ocean circulation patterns in the North Atlantic and North Pacific oceans.
For the same reason, flows of air down toward the northern surface of the Earth tend to spread across the surface in a clockwise pattern. Thus, clockwise air circulation is characteristic of high pressure weather cells in the Northern Hemisphere. Conversely, air rising from the northern surface of the Earth (creating a region of low pressure) tends to draw air toward it in a counterclockwise pattern. Hurricanes and tropical storms (massive low-pressure systems) spin counter-clockwise in the Northern Hemisphere.
The shadow of a sundial moves clockwise in the Northern Hemisphere (opposite of the Southern Hemisphere). During the day, the Sun tends to rise to its maximum at a southerly position.
When viewed from the Northern Hemisphere, the Moon appears inverted compared to a view from the Southern Hemisphere. The North Pole faces away from the galactic center of the Milky Way. This results in the Milky Way being sparser and dimmer in the Northern Hemisphere compared to the Southern Hemisphere, making the Northern Hemisphere more suitable for deep-space observation, as it is not "blinded" by the Milky Way.
The Northern Hemisphere is home to approximately 6.57 billion persons which is around 80/88-90% of the earth's total human population of 7.3 billion persons, possibly due to high fertility rates.
List of continents
- All of continental Europe excluding overseas territories in the Southern Hemisphere and Eastern Hemisphere
- All of North America, Central America and the Caribbean excluding overseas territories
- The vast majority of Asia, except East Timor, and part of Indonesia (which straddles the equator)
- About ⅔ of Africa, just above the “horn”
- About ¹⁄10 of South America, north of the mouth of the Amazon River
- Report of the IAU Working Group on cartographic coordinates and rotational elements: 2009
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- "Perspective of the Moon from the Northern and Southern Hemispheres". Retrieved 22 October 2013.
- "90% Of People Live In The Northern Hemisphere - Business Insider". Business Insider. 4 May 2012. Retrieved 10 November 2015.
- "GIC - Article". galegroup.com. Retrieved 10 November 2015.
Media related to Northern Hemisphere at Wikimedia Commons