small ice - определение. Что такое small ice
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Что (кто) такое small ice - определение

PERIOD OF COOLING THAT OCCURRED AFTER THE MEDIEVAL WARM PERIOD, USUALLY DEFINED AS BETWEEN THE 16TH TO THE 19TH CENTURIES
Little ice age; Mini-ice age; Small Ice Age; Mini ice age; The little ice age; The Little Ice Age; Micro ice age
  • url-status=live }} ("The data show that the modern period is very different to what occurred in the past. The often quoted Medieval Warm Period and Little Ice Age are real phenomena, but small compared to the recent changes.")</ref>
  • Winter skating on the main canal of Pompenburg, [[Rotterdam]] in 1825, shortly before the minimum, by Bartholomeus Johannes van Hove
  • cosmogenic isotope]] in tree trunks. The second panel shows the winter values of [[Central England Temperature]], being the mean for December, January and February. The third panel shows the summer values, being the mean for June, July and August. The bottom panel gives the aerosal [[optical depth]], showing volcanic dust levels, from ice sheet cores. The vertical mauve lines are years in which frost fairs were held on the Thames in London and the vertical orange lines are the years when the ice there was reported as thick enough to walk on. The first cyan line is the date of the removal of the old [[London Bridge]] and wier and the second is the completion of the embankments: both riverine developments that increased the flow and ended Thames freezing events. All data sources are given in reference <ref name="lock1" />
  • 1608}}, [[Hendrick Avercamp]]
  • Norse]] Greenlanders are from a 1408 marriage at [[Hvalsey Church]], which is now the best-preserved Norse ruin.
  • ''Patterdale Landscape with Cattle'' (1833) by John Glover depicts agricultural practices like pastoralism, which contributed to the aridification of Australia's late Little Ice Age.
  • {{CO2}} mixing ratios at [[Law Dome]]
  • "February" from the calendar of [[Les Très Riches Heures du duc de Berry]], 1412–1416
  • Sunspot number compared with Northern Hemisphere (NH) temperature anomaly. The upper panel shows 11-year smoothed group sunspot numbers from telescopic observations and the sunspot number derived from carbon-14 cosmogenic isotope abundances in tree trunks. The lower panel shows the Northern Hemisphere (NH) temperature anomaly (relative to the 1990 level) from a wide variety of paleoclimate proxies: the black line is the mean value, and the colors give the uncertainty probability distribution. The blue dots are the instrumental record. The dashed lines mark the start and end of the Little Ice Age (LIA) defined by the (NH) temperature anomaly level -0.16 degrees Celsius. All data sources are described in references <ref name="owens1"/> and <ref name="lock1"/>
  • Thermohaline circulation or Oceanic conveyor belt illustrated
  • ''[[The Hunters in the Snow]]'' by [[Pieter Brueghel the Elder]], 1565
  • The Maunder Minimum in a 400-year history of sunspot numbers
  • ''The Frozen Thames'', 1677
  • The Reverend Robert Walker Skating on Duddingston Loch]]'', attributed to [[Henry Raeburn]], 1790s
  • [[March Across the Belts]], 1658
Найдено результатов: 4756
small intestine         
  • Absorption of glucose in the small intestine
  • This cross section diagram shows the 4 layers of the small intestine wall.
  • [[Micrograph]] of the small intestine [[mucosa]] showing the [[intestinal villi]] and [[crypts of Lieberkühn]].
PART OF THE DIGESTIVE TRACT, FOLLOWING THE STOMACH AND FOLLOWED BY THE LARGE INTESTINE FAKE
Small bowel; Small Intestine; Small intestinal; Small intestines; Intestine, small; Unstirred water layer; Intestinum tenue; Absorption (small intestine)
¦ noun the part of the intestine that runs between the stomach and the large intestine, consisting of the duodenum, the jejunum, and the ileum.
Small molecule         
MOLECULE THAT WEIGHS LESS THAN 800 DALTON
Small Molecule; Small molecule anti-genomic therapeutics; Small molecules; Small-molecule; Small organic compound; Non-peptide; Nonpeptide; Small-molecule drug
Within the fields of molecular biology and pharmacology, a small molecule or micromolecule is a low molecular weight (≤ 1000 daltons) organic compound that may regulate a biological process, with a size on the order of 1 nm. Many drugs are small molecules; the terms are equivalent in the literature.
Ice Ih         
HEXAGONAL CRYSTAL FORM OF ORDINARY ICE
Ice I; Hexagonal ice; Ice-Ih; Ice 1h; Ice one; Ice-one; Ice one h
[showing details of an ice cube under magnification. Ice Ih is the form of ice commonly seen on Earth.
Ice VI         
TETRAGONAL FORM OF ICE
Ice 6; Ice six; Ice-six
Ice VI is a form of ice that exists at high pressure at the order of about 1 GPa (= 10 000 bar) and temperatures ranging from 130 up to 355 Kelvin (−143 °C up to 82 °C); see also the phase diagram of water. Its discovery and the discovery of other high-pressure forms of water were published by P.
Ice dune         
DUNE MADE OF ICE
Ice-foot; Ice ridge; Ice foot
An ice dune, also called an ice ridge or an ice foot, is a formation of ice that accumulates on the shores of many arctic beaches and is also common along the shores of the Great Lakes during the winter.French 2007, p.
Small dodecicosidodecahedron         
  • 3D model of a small dodecacronic hexecontahedron
  • 3D model of a small dodecicosidodecahedron
POLYHEDRON WITH 44 FACES
Small dodecacronic hexecontahedron; Saddid; Small dodekicosidodecahedron
In geometry, the small dodecicosidodecahedron (or small dodekicosidodecahedron) is a nonconvex uniform polyhedron, indexed as U33. It has 44 faces (20 triangles, 12 pentagons, and 12 decagons), 120 edges, and 60 vertices.
Ice V         
MONOCLINIC FORM OF ICE
Ice 5; Ice five; Ice-five
Ice V, pronounced "ice five", is a monoclinic crystalline phase of water, formed by cooling water to 253 K at 500 MPa. It has a density of 1.
Ice VII         
STABLE CUBIC CRYSTALLINE VARIANT OF ICE
Ice 7; Ice seven; Ice-seven
Ice VII is a cubic crystalline form of ice. It can be formed from liquid water above 3 GPa (30,000 atmospheres) by lowering its temperature to room temperature, or by decompressing heavy water (D2O) ice VI below 95 K.
Ice XI         
  • Crystal structure of ice XI (c-axis in the vertical direction)
ORTHORHOMBIC FORM OF ICE
Ice 11; Ice eleven; Ice-eleven; Ferroelectric ice
Ice XI is the hydrogen-ordered form of Ih, the ordinary form of ice. Different phases of ice, from ice II to ice XVIII, have been created in the laboratory at different temperatures and pressures.
Thiele/Small parameters         
SET OF ELECTROMECHANICAL PARAMETERS
T/S Parameters; Thiele Small parameters; Thiele small parameters; Thiele small; THIEL; Thiel/Small; Thiele-Small parameters; Thiele/Small
Thiele/Small parameters (commonly abbreviated T/S parameters, or TSP) are a set of electromechanical parameters that define the specified low frequency performance of a loudspeaker driver. These parameters are published in specification sheets by driver manufacturers so that designers have a guide in selecting off-the-shelf drivers for loudspeaker designs.

Википедия

Little Ice Age

The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. The period has been conventionally defined as extending from the 16th to the 19th centuries, but some experts prefer an alternative timespan from about 1300 to about 1850.

The NASA Earth Observatory notes three particularly cold intervals. One began about 1650, another about 1770, and the last in 1850, all of which were separated by intervals of slight warming. The Intergovernmental Panel on Climate Change Third Assessment Report considered that the timing and the areas affected by the Little Ice Age suggested largely independent regional climate changes, rather than a globally synchronous increased glaciation. At most, there was modest cooling of the Northern Hemisphere during the period.

Several causes have been proposed: cyclical lows in solar radiation, heightened volcanic activity, changes in the ocean circulation, variations in Earth's orbit and axial tilt (orbital forcing), inherent variability in global climate, and decreases in the human population (such as from the Black Death and the epidemics emerging in the Americas upon European contact).