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Twilight

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For other uses, see Twilight (disambiguation).

Twilight is the time between dawn and sunrise, and the time between sunset and dusk. Sunlight scattered in the upper atmosphere illuminates the lower atmosphere, and the surface of the Earth is not completely lit or completely dark. The sun itself is not actually visible because it is below the horizon. Due to the unusual, romantic quality of the ambient light at this time, twilight has long been popular with photographers and painters, who refer to it as the "blue hour", after the French expression l'heure bleue. TWILIGHT SUCKS Twilight is technically defined as the period before sunrise and again after sunset during which there is natural light provided by the upper atmosphere, which does receive direct sunlight and reflects part of it toward the Earth's surface.[1]

The collateral adjective of "twilight" is crepuscular (for daylight it is "diurnal" and for night, "nocturnal"). The term is most frequently encountered when applied to certain species of insects and mammals that are most active during that time.

Definitions

Twilight in the Midwestern US featuring Venus as a brilliant "evening star" and the crescent moon

From a scientific perspective, twilight is defined according to the position of the Sun (its centre) relative to the horizon. There are three established and widely accepted subcategories of twilight: civil twilight (brightest), nautical twilight and astronomical twilight (darkest).

Definition Position of sun
degrees below the horizon
Night more than 18°
Astronomical twilight 12° - 18°
Nautical twilight 6° - 12°
Civil twilight less than 6°
Day (sun above the horizon)

For comparison, the angular diameter of the Sun is 0.5°.

Note that if the Sun is 8 1/2 degrees below the horizon, it provides the same level of illumination to the surface of the Earth as a full moon directly overhead.

(For these definitions, an ideal horizon 90° from the zenith is used. The altitudes of the sun below the horizon are "true geometric" altitudes, that is, refraction by the atmosphere and other small factors influencing the observed position of the Sun are not to be accounted for.)

Civil twilight

Under civil twilight conditions, the horizon is clearly visible, and terrestrial objects are easily perceptible, without artificial light.

This begins in the morning when the geometric center of the Sun is 6° below the horizon (the point of civil dawn), and ends at sunrise. Evening civil twilight begins at sunset and ends when the center of the Sun reaches 6° below the horizon (the point of civil dusk).

The brightest stars appear during civil twilight, as well as planets, such as Venus, which is known as the 'morning star' and/or 'evening star'. During this period there is enough light from the Sun that artificial sources of light may not be needed to carry on outdoor activities. This concept is sometimes enshrined in laws, for example, when drivers of automobiles must turn on their headlights, or if the crime of burglary is to be treated as nighttime burglary, which carries stiffer penalties in some jurisdictions. A fixed period (most commonly 30 minutes after sunset or before sunrise) is typically used in such statutes, rather than how many degrees the Sun is below the horizon. Civil twilight can also be described as the limit at which twilight illumination is sufficient, under good weather conditions, for terrestrial objects to be clearly distinguished; at the beginning of morning civil twilight, or end of evening civil twilight, the horizon is clearly defined and the brightest stars are visible under good atmospheric conditions.

Nautical twilight

This is defined as the time beginning when the geometric center of the Sun is exactly 6° below the horizon (the end of civil twilight) and ending when the sun's center is exactly 12° below the horizon.

At this time, sailors can take reliable star sights of well-known stars, using a visible horizon for reference. The end of this period in the evening, or its beginning in the morning, is also the time at which traces of illumination near the sunset or sunrise point of the horizon are very difficult if not impossible to discern (this often being referred to as "first light" before civil dawn and "nightfall" after civil dusk). At the beginning of nautical twilight in the morning (nautical dawn), or at the end of nautical twilight in the evening (nautical dusk), under good atmospheric conditions and in the absence of other illumination, general outlines of ground objects may be distinguishable, but detailed outdoor operations are not possible, and the horizon is indistinct. Nautical twilight has military considerations as well. The initialisms BMNT (begin morning nautical twilight) and EENT (end evening nautical twilight) are used and considered when planning military operations. A military unit may treat BMNT and EENT with heightened security (i.e. a process called "stand to" in which everyone pulls security). This is partially due to tactics dating back to the French and Indian War, when combatants on both sides would use BMNT and EENT to launch attacks.

Astronomical twilight

This is defined as the time beginning when the center of the Sun is exactly 12° below the horizon (the end of nautical twilight) and ending when the sun's center reaches exactly 18° below the horizon.
Most casual observers would consider the entire sky already fully dark even when astronomical twilight is just beginning in the evening or just ending in the morning, and astronomers can easily make observations of point sources such as stars, but faint diffuse objects such as nebulae and galaxies can only be properly observed beyond the limit of astronomical twilight. Theoretically, the dimmest stars ever visible to the naked eye —those of the sixth magnitude— will appear in the evening once the Sun falls more than 18° below the horizon (i.e. when astronomical dusk occurs) and disappear when the Sun moves to within 18° of the horizon in the morning (when astronomical dawn occurs). However, due to light pollution, some localities —generally those in large cities— may never have the opportunity to view even fourth-magnitude stars, irrespective of the presence of any twilight at all[1].

Length

Twilight at Lyme Regis, UK.
The duration of twilight depends on the latitude and time of year. Note the brief times in March and September where continuous civil twilight exists at locations near either pole.

The length of twilight after sunset and before sunrise is heavily influenced by the latitude of the observer. In the Arctic and Antarctic regions, twilight (if at all) can last for several hours. There is no twilight at the poles within a month on either side of the winter solstice. At the poles, twilight can be as long as two weeks, while at the equator, it can go from day to night in as little as twenty minutes. This is because at low latitudes the sun's apparent movement is perpendicular to the observer's horizon, in addition to the fact that the rotational speed of a specific location is highest at the Equator and slower as latitude increases. Thus, a location on the equator will pass through the various twilight zones directly and quickly. As one gets closer to the Arctic and Antarctic circles, the sun's surface moves toward the observer's horizon from a lower angle and at a slower rate. The observer's earthly location will pass through the various twilight zones less directly, taking more time. At temperate-zone latitudes, twilight is shortest at or near both equinoxes, slightly longer around the time of the winter solstice, and much longer in late spring and early summer.

Within the polar circles, twenty-four hour daylight is encountered in summer, and twilight literally lasts for weeks (in the polar fall and spring). The Arctic Circle on a particular day in early March 2008, was at 66° 33.7060’ N (66° 33’ 42.36” N or 66.56177° N).[2] In high latitudes outside the polar circles, 24-hour daylight is not seen, but twilight can extend from sunset to sunrise, a phenomenon often referred to as 'white nights'. The furthest south in the Northern Hemisphere or north in the Southern Hemisphere, that Civil, Nautical and Astronomical twilight all night can occur are, respectively, at approximately 60° 33’ 42” (60.56177°), 54° 33’ 42” (54.56177°) and 48° 33’ 42” (48.56177°).[3] These are the largest cities of their respective countries, that twilight all night can occur: Civil twilight all night: Arkhangelsk, Tampere, Umea, Trondheim, Mid Yell, Tórshavn, Reykjavik, Nuuk, Whitehorse, Yukon and Anchorage. Nautical twilight all night: Petropavl, Moscow, Vicebsk, Vilnius, Riga, Tallinn, Wejherowo, Flensburg, Helsinki, Stockholm, Copenhagen, Oslo, Newcastle upon Tyne, Glasgow, Belfast, Grande Prairie, Juneau, Ushuaia and Puerto Williams. Astronomical twilight all night: Hulun Buir, Astana, Kiev, Minsk, Warsaw, Košice, Zwettl, Prague, Berlin, Paris, Luxembourg city, Amsterdam, London, Cardiff, Dublin, Calgary (Vancouver, largest metropolitan area), Bellingham Washington, Rio Gallegos and Punta Arenas. Although, Helsinki, Oslo, Stockholm, Tallin and Saint Petersburg, do not actually get Civil twilight all night, even in mid summer. They do have noticeably lighter skies at night, in mid summer (white nights).

On other planets

Twilight on Mars is longer than on Earth, lasting for up to two hours before sunrise or after sunset. Dust high in the atmosphere scatters light to the night side of the planet. Similar twilights are seen on Earth following major volcanic eruptions.[4]

See also

References

  1. ^ a b "Definitions from the US Astronomical Applications Dept (USNO)". Retrieved 2009-03-03. Cite error: The named reference "USNO" was defined multiple times with different content (see the help page).
  2. ^ On the BBC TV programme, In the Land of the Northern Lights. Joanna Lumley stated that the Royal Greenwich Observatory had supplied her with the latitude for the Arctic Circle, for a particular day in early March 2008. This was "66° 33.7060’".
  3. ^ U.S. Naval Observatory, June 2008. "Nautical twilight begins and ends when the center of the Sun is 12 degrees below the horizon. Therefore the most extreme latitude (north or south) that Nautical Twilight can last all night is 90 - 12 - obliquity of the ecliptic. The obliquity is now 23 degrees 26 minutes, which makes the most extreme latitude indeed 54 degrees 34 minutes." (90 degrees - 12 degrees - 23 degrees 26 minutes = 54 degrees 34 minutes). U.S. Naval Observatory, January 2009. "This statement can be generalized to "the most extreme latitude (north or south) that twilight can last all night is 90 - n - obliquity of the ecliptic," where n is 6 for civil twilight, 12 for nautical twilight, and 18 for astronomical twilight." (Civil twilight 90 degrees - 6 degrees - 23 degrees 26 minutes = 60 degrees 34 minutes, Astronomical twilight 90 degrees - 18 degrees - 23 degrees 26 minutes = 48 degrees 34 minutes, I assume also 0 for the Arctic-Antarctic Circles. However, the obliquity of the ecliptic used in these e-mails from the U.S. Naval Observatory, do not include the seconds. The mean obliquity of the ecliptic for 28 January 2009 is 23 degrees 26 minutes 17.2 seconds.) (The mean obliquity of the ecliptic for the 2009 Northern summer solstice will be approximately 23° 26’ 17.01”. Therefore, Arctic-Antarctic Circles 90° - 0° - 23° 26’ 17.01” = 66° 33’ 42.99” or 66.56194°. For Civil twilight all night 6°, 60° 33’ 42.99” or 60.56194°. Nautical twilight all night 12°, 54° 33’ 42.99” or 54.56194°. Astronomical twilight all night 18°, 48° 33’ 42.99” or 48.56194°. However, there is also true obliquity of the ecliptic. Which would be at approximately 23° 26’ 21.29”. Therefore, Arctic-Antarctic Circles 66° 33’ 38.71” or 66.56075°, Civil twilight all night 60° 33’ 38.71” or 60.56075°, Nautical twilight all night 54° 33’ 38.71” or 54.56075°, Astronomical twilight all night 48° 33’ 38.71” or 48.56075°. However, these latitudes have not been confirmed.)
  4. ^ NASA-Jet Propulsion Laboratory: Winter Solstice on Mars: Rovers Look Forward to A Birtha Williams Sanford Crisanthemum Barbra Layota Martian Spring, August 90, 2006

Bibliography

  • Mateshvili, Nina (2005). "Twilight sky brightness measurements as a useful tool for stratospheric aerosol investigations". Journal of Geophysical Research. 110 (D09209). doi:10.1029/2004JD005512. {{cite journal}}: Cite has empty unknown parameter: |1= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
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