NATURAL SCIENCE
Nature, in the broadest sense, is equivalent to the natural world, physical world, or material world. "Nature" refers to the
phenomena of the physical world, and also to
life in general. It ranges in scale from the
subatomic to the
cosmic.
The word nature is derived from the
Latin word natura, or "essential qualities, innate disposition", and in ancient times, literally meant "birth". Natura was a Latin translation of the Greek word
physis (φύσις), which originally related to the intrinsic characteristics that plants, animals, and other features of the world develop of their own accord. The concept of nature as a whole, the physical
universe, is one of several expansions of the original notion; it began with certain core applications of the word φύσις by
pre-Socratic philosophers, and has steadily gained currency ever since. This usage was confirmed during the advent of modern
scientific method in the last several centuries.
Within the various uses of the word today, "nature" often refers to
geology and
wildlife. Nature may refer to the general realm of various types of living plants and animals, and in some cases to the processes associated with inanimate objects – the way that particular types of things exist and change of their own accord, such as the
weather and
geology of the Earth, and the
matter and
energy of which all these things are composed. It is often taken to mean the "
natural environment" or
wilderness–wild animals, rocks, forest, beaches, and in general those things that have not been substantially altered by human intervention, or which persist despite human intervention. For example, manufactured objects and human interaction generally are not considered part of nature, unless qualified as, for example, "human nature" or "the whole of nature". This more traditional concept of natural things which can still be found today implies a distinction between the natural and the artificial, with the artificial being understood as that which has been brought into being by a human
consciousness or a human
mind. Depending on the particular context, the term "natural" might also be distinguished from the
unnatural, the
supernatural, or
synthetic.
It is capitalized when used as a proper noun, as in 'the nature of Nature'.
RIVER
A
river is a natural
watercourse, usually
freshwater, flowing toward an
ocean, a
lake, a
sea or another river. In a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. Small rivers may also be called by several other names, including
stream, creek, brook, rivulet, and rill; there is no general rule that defines what can be called a river. Many names for small rivers are specific to geographic location; one example is Burnin Scotland and North-east England. Sometimes a river is said to be larger than a creek, but this is not always the case, due to vagueness in the language. A river is part of the
hydrological cycle. Water within a river is generally collected from
precipitation through
surface runoff,
groundwaterrecharge,
springs, and the release of stored water in natural ice and snowpacks (i.e., from
glaciers).
NATURAL EARTH
Natural
Earth (or, "the earth") is the only
planet presently known to support life, and its natural features are the subject of many fields of scientific research. Within the
solar system, it is third closest to the sun; it is the largest
terrestrial planet and the fifth largest overall. Its most prominent climatic features are its two large polar regions, two relatively narrow
temperate zones, and a wide
equatorial tropical to
subtropical region.
Precipitation varies widely with location, from several metres of water per year to less than a millimetre. 71 percent of the Earth's surface is covered by salt-water oceans. The remainder consists of continents and islands, with most of the inhabited land in the
Northern Hemisphere.
Earth has evolved through geological and biological processes that have left traces of the original conditions. The
outer surface is divided into several gradually migrating
tectonic plates. The interior remains active, with a thick layer of plastic
mantle and an iron-filled core that generates a
magnetic field.
The
atmospheric conditions have been significantly altered from the original conditions by the presence of life-forms, which create an ecological balance that stabilizes the surface conditions. Despite the wide regional variations in climate by
latitude and other geographic factors, the long-term average global climate is quite stable during interglacial periods, and variations of a degree or two of average global temperature have historically had major effects on the ecological balance, and on the actual geography of the Earth.
ATMOSPHERE, CLIMATE AND WEATHER
The atmosphere of the Earth serves as a key factor in sustaining the planetary
ecosystem. The thin layer of
gases that envelops the Earth is held in place by the planet's gravity. Dry
air consists of 78%
nitrogen, 21%
oxygen, 1%
argon and other
inert gases, carbon dioxide, etc.; but air also contains a variable amount of
water vapor. The atmospheric pressure declines steadily with altitude, and has a
scale height of about 8 kilometres at the Earth's surface: the height at which the atmospheric pressure has declined by a factor of
e (a mathematical constant equal to 2.71...)The
ozone layer of the Earth's atmosphere plays an important role in depleting the amount of
ultraviolet (UV) radiation that reaches the surface. As
DNA is readily damaged by UV light, this serves to protect life at the surface. The atmosphere also retains heat during the night, thereby reducing the daily temperature extremes.
Terrestrial weather occurs almost exclusively in the
lower part of the atmosphere, and serves as a convective system for redistributing heat.
Ocean currents are another important factor in determining climate, particularly the major underwater
thermohaline circulation which distributes heat energy from the equatorial oceans to the polar regions. These currents help to moderate the differences in
temperature between winter and summer in the temperate zones. Also, without the redistributions of heat energy by the ocean currents and atmosphere, the tropics would be much hotter, and the
polar regions much colder.
Weather can have both beneficial and harmful effects. Extremes in weather, such as
tornadoes or
hurricanes and
cyclones, can expend large amounts of energy along their paths, and produce devastation. Surface vegetation has evolved a dependence on the seasonal variation of the weather, and sudden changes lasting only a few years can have a dramatic effect, both on the vegetation and on the animals which depend on its growth for their food.
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The planetary climate is a measure of the long-term trends in the weather. Various factors are known to influence the climate, including ocean currents, surface albedo, greenhouse gases, variations in the solar luminosity, and changes to the planet's orbit. Based on historical records, the Earth is known to have undergone drastic climate changes in the past, including ice ages.
The climate of a region depends on a number of factors, especially latitude. A latitudinal band of the surface with similar climatic attributes forms a climate region. There are a number of such regions, ranging from the tropical climate at the equator to the polar climate in the northern and southern extremes. Weather is also influenced by theseasons, which result from the Earth's axis being tilted relative to its orbital plane. Thus, at any given time during the summer or winter, one part of the planet is more directly exposed to the rays of the sun. This exposure alternates as the Earth revolves in its orbit. At any given time, regardless of season, the northern and southern hemispheres experience opposite seasons.
Weather is a chaotic system that is readily modified by small changes to the environment, so accurate weather forecasting is currently limited to only a few days.[citation needed] Overall, two things are currently happening worldwide: temperature is increasing on the average; and regional climates have been undergoing noticeable changes.
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WATER ON EARTH
Water is a
chemical substance that is composed of
hydrogen and
oxygen and is vital for all known forms of
life. In typical usage, waterrefers only to its
liquid form or
state, but the substance also has a
solid state,
ice, and a
gaseous state,
water vapor or
steam. Water covers 71% of the
Earth's surface. On Earth, it is found mostly in oceans and other large water bodies, with 1.6% of water below ground in
aquifers and 0.001% in the
air as
vapor,
clouds (formed of solid and liquid water particles suspended in air), and
precipitation.
Oceans hold 97% of surface water,
glaciers and polar
ice caps 2.4%, and other land surface water such as
rivers,
lakes and
ponds 0.6%. Additionally, a minute amount of the Earth's water is contained within biological bodies and manufactured products.