Isis (disambiguation)

Isis is a goddess from the polytheistic pantheon of Egypt.

Isis or ISIS may also refer to:

Organisations

Non-profits

Isis (band)

Isis (stylized as ISIS) was a Los Angeles-based post-metal band, founded in Boston, Massachusetts, with a career spanning from 1997 to 2010. They borrowed from and helped to evolve a sound pioneered by the likes of Neurosis and Godflesh, creating heavy music consisting of lengthy songs that focus on repetition and evolution of structure.

The band's last album, Wavering Radiant, was released on 5 May 2009. They disbanded in June 2010, just before the release of a split EP with the Melvins.

History

Formation and early releases (1997–2001)

Goa'uld characters in Stargate

This is a list of the Goa'uld characters that appear in Stargate, Stargate SG-1, and Stargate Atlantis. In the Stargate fictional universe, the Goa'uld are a parasitic alien race that use other beings as hosts. Ra had stated in the original Stargate film that he had used humans exclusively as hosts for millennia, because Goa'uld technology can repair human bodies so easily that by inhabiting human forms they can be in effect ageless, though they can still be injured or killed. Most Goa'uld pose as gods in order to control slave armies, and are considered evil, egocentric megalomaniacs by those who do not worship them. The Goa'uld are extremely intelligent and have an aptitude for understanding, working with, and using technology that is superior to that of humans. They each have full access to their species' genetic memory from the moment of birth. As a result, no Goa'uld has to learn how to operate any technological device; they 'know' how to do so innately.

Maritime

Maritime is primarily an adjective that describes objects or activities related to the sea.

Maritime or Maritimes as a noun may also refer to:

Geography

Music

See also

Related terms

Climate categories in viticulture

In viticulture, the climates of wine regions are categorised based on the overall characteristics of the area's climate during the growing season. While variations in macroclimate are acknowledged, the climates of most wine regions are categorised (somewhat loosely based on the Köppen climate classification) as being part of a Mediterranean (for example Tuscany), maritime (ex: Bordeaux) or continental climate (ex: Columbia Valley). The majority of the world's premium wine production takes place in one of these three climate categories in locations between the 30th parallel and 50th parallel in both the northern and southern hemisphere. While viticulture does exist in some tropical climates, most notably Brazil, the amount of quality wine production in those areas is so small that the climate effect has not been as extensively studied as other categories.

Influence of climate on viticulture

Beyond establishing whether or not viticulture can even be sustained in an area, the climatic influences of a particular area goes a long way in influencing the type of grape varieties grown in a region and the type of viticultural practices that will be used. The presence of adequate sun, heat and water are all vital to the healthy growth and development of grapevines during the growing season. Additionally, continuing research has shed more light on the influence of dormancy that occurs after harvest when the grapevine essentially shuts down and reserves its energy for the beginning of the next year's growing cycle.

Oceanic climate

An oceanic climate (also known as marine, west coast and maritime) is the climate typical of the west coasts at the middle latitudes of continents, and generally features warm (but not hot) summers and cool (but not cold) winters, with a relatively narrow annual temperature range. It typically lacks a dry season, as precipitation is more evenly dispersed throughout the year. It is the predominant climate type across much of Northern Western Europe, parts of the Appalachians, portions of southwestern South America and small areas of Africa, in southeast Australia, and New Zealand as well as isolated locations elsewhere.

Under the Köppen climate classification, the typical zone associated with the Oceanic climate is Cfb, although it includes subtropical highland zones not usually associated with marine climates. Often, parts of the Csb Mediterranean or Dry-Summer subtropical zones are not associated with a typical Mediterranean climate, and would be classified as Temperate Oceanic (Cfb), except dry-summer patterns meet Köppen's minimum Cs thresholds. Other climate classification systems, such as Trewartha climate classification, place these areas firmly in the Oceanic zone (Do).