Nature Geoscience

Nature Geoscience is a monthly peer-reviewed scientific journal published by the Nature Publishing Group. The editor-in-chief is Heike Langenberg. It was established in January 2008.

Nature Geoscience
Nature Geoscience cover
DisciplineGeosciences
LanguageEnglish
Edited byHeike Langenberg
Publication details
Publication history
2008-present
Publisher
FrequencyMonthly
13.941
Standard abbreviations
Nat. Geosci.
Indexing
CODENNGAEBU
ISSN1752-0894 (print)
1752-0908 (web)
LCCN2008203703
OCLC no.187319519
Links

Scope

The journal covers all aspects of the Earth sciences, including theoretical research, modelling, and field work. Significant related work in other fields, such as atmospheric sciences, geology, geophysics, climatology, oceanography, palaeontology, and space science, is also published. [1]

Abstracting and indexing

The journal is abstracted and indexed by:[2][3][4][5]

According to the Journal Citation Reports, the journal has a 2016 impact factor of 13.941.[6]

See also

References

  1. ^ "About the journal". Nature Geoscience. Nature Publishing Group. Retrieved 2011-07-30.
  2. ^ "Nature Geoscience". Master Journal List. Thomson Reuters. Retrieved 2011-07-30.
  3. ^ "CAS Source Index (CASSI)" (Online description). American Chemical Society. Retrieved 2011-07-30.
  4. ^ "GeoRef" (PDF). EBSCO. Retrieved 2011-07-30.
  5. ^ "CAB Abstracts". CAB International. Retrieved 2011-07-30.
  6. ^ "Nature Geoscience". 2016 Journal Citation Reports. Web of Science (Science ed.). Thomson Reuters. 2017. (subscription required)

External links

2013 in Antarctica

Events from the year 2013 in Antarctica

Aeolis Mensae

Aeolis Mensae is tableland feature in the Aeolis quadrangle of Mars. Its location is centered at 2.9° south latitude and 219.6° west longitude. It is 820 kilometres (510 mi) long and was named after a classical albedo feature name.

Aggradation

Aggradation (or alluviation) is the term used in geology for the increase in land elevation, typically in a river system, due to the deposition of sediment. Aggradation occurs in areas in which the supply of sediment is greater than the amount of material that the system is able to transport. The mass balance between sediment being transported and sediment in the bed is described by the Exner equation.

Typical aggradational environments include lowland alluvial rivers, river deltas, and alluvial fans. Aggradational environments are often undergoing slow subsidence which balances the increase in land surface elevation due to aggradation. After millions of years, an aggradational environment will become a sedimentary basin, which contains the deposited sediment, including paleochannels and ancient floodplains.

Aggradation can be caused by changes in climate, land use, and geologic activity, such as volcanic eruption, earthquakes, and faulting. For example, volcanic eruptions may lead to rivers carrying more sediment than the flow can transport: this leads to the burial of the old channel and its floodplain. In another example, the quantity of sediment entering a river channel may increase when climate becomes drier. The increase in sediment is caused by a decrease in soil binding that results from plant growth being suppressed. The drier conditions cause river flow to decrease at the same time as sediment is being supplied in greater quantities, resulting in the river becoming choked with sediment.

In 2009, a report by researchers from the University of Colorado at Boulder in the journal Nature Geoscience said that reduced aggradation was contributing to an increased risk of flooding in many river deltas.

Calcium–aluminium-rich inclusion

A calcium–aluminium-rich inclusion or Ca–Al-rich inclusion (CAI) is a submillimeter- to centimeter-sized light-colored calcium- and aluminium-rich inclusion found in carbonaceous chondrite meteorites. They are probably the oldest substances in the Solar System. The oldest age was measured in an inclusion of the CV3 carbonaceous chondrite Northwest Africa (NWA) 2364 and was dated at 4568.22 ± 0.17 Mya.

Climate of Antarctica

The climate of Antarctica is the coldest on Earth. The lowest air temperature record on Antarctica was set on 21 July 1983, when −89.2 °C (−128.6 °F) was observed at Vostok Station. Satellite measurements have identified even lower ground temperatures, with −93.2 °C (−135.8 °F) having been observed at the cloud-free East Antarctic Plateau on 10 August 2010.The continent is also extremely dry (it is technically a desert), averaging 166 mm (6.5 in) of precipitation per year. Snow rarely melts on most parts of the continent, and, after being compressed, becomes the glacier ice that makes up the ice sheet. Weather fronts rarely penetrate far into the continent, because of the katabatic winds. Most of Antarctica has an ice-cap climate (Köppen classification EF) with very cold, generally extremely dry weather.

Cryogenian

The Cryogenian ( , from Greek κρύος (krýos), meaning "cold" and γένεσις (génesis), meaning "birth") is a geologic period that lasted from 720 to 635 million years ago. It forms the second geologic period of the Neoproterozoic Era, preceded by the Tonian Period and followed by the Ediacaran.

The Sturtian and Marinoan glaciations occurred during the Cryogenian period, which are the greatest ice ages known to have occurred on Earth. These events are the subject of much scientific controversy. The main debate contests whether these glaciations covered the entire planet (the so-called "Snowball Earth") or a band of open sea survived near the equator (termed "slushball Earth").

Earth's outer core

Earth's outer core is a fluid layer about 2,400 km (1,500 mi) thick and composed of mostly iron and nickel that lies above Earth's solid inner core and below its mantle. Its outer boundary lies 2,890 km (1,800 mi) beneath Earth's surface. The transition between the inner core and outer core is located approximately 5,150 km (3,200 mi) beneath the Earth's surface. Unlike the inner core, the outer core is liquid. The inner core is also referred to as the solid core.

Glacial period

A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The last glacial period ended about 15,000 years ago. The Holocene epoch is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state.

Global warming in Antarctica

The effects of global warming in Antarctica may include rising temperatures and increasing snow melt and ice loss. A summary study in 2018 incorporating calculations and data from many other studies estimated that total ice loss was 43 gigatons per year on average during the period from 1992 to 2002 but has accelerated to an average of 220 gigatons per year during the five years from 2012 to 2017.

Katrin Meissner (scientist)

Katrin Juliane Meissner is a German and Australian physical oceanographer and climate scientist.Meissner completed an engineering degree at the Ecole Centrale de Lille in 1995, a Diplôme d'Etudes Approfondies, at the Université Pierre et Marie Curie, Paris VI, France in 1996, and a Doctor of Physics (PhD) at the Universität Bremen, Germany in 1999. In 2000, she received the Annette Barthelt Prize for outstanding research in the field of marine science.

Late Antique Little Ice Age

The Late Antique Little Ice Age was a long-lasting Northern Hemisphere cooling period in the 6th and 7th century AD, during the period known as late antiquity.

Marinoan glaciation

The Marinoan glaciation was a period of worldwide glaciation that lasted from approximately 650 to 635 Ma (million years ago) during the Cryogenian period. The glaciation may have covered the entire planet, in an event called the Snowball Earth. The end of the glaciation may have been sped by the release of methane from equatorial permafrost.

Maunder Minimum

The Maunder Minimum, also known as the "prolonged sunspot minimum", is the name used for the period around 1645 to 1715 during which sunspots became exceedingly rare, as was then noted by solar observers.

The term was introduced after John A. Eddy published a landmark 1976 paper in Science. Astronomers before Eddy had also named the period after the solar astronomers Annie Russell Maunder (1868–1947) and her husband, Edward Walter Maunder (1851–1928), who studied how sunspot latitudes changed with time. The period which the spouses examined included the second half of the 17th century.

Two papers were published in Edward Maunder's name in 1890 and 1894, and he cited earlier papers written by Gustav Spörer. Because Annie Maunder had not received a university degree, restrictions at the time caused her contribution not to be publicly recognized.Spörer noted that, during a 28-year period (1672–1699) within the Maunder Minimum, observations revealed fewer than 50 sunspots.

This contrasts with the typical 40000 – 50000 sunspots seen in modern times (over similar 25 year sampling).Like the Homeric Minimum, Dalton Minimum and the Spörer Minimum, the Maunder Minimum coincided with a period of lower-than-average European temperatures.

Nature Neuroscience

Nature Neuroscience is a monthly scientific journal published by Nature Publishing Group. Its focus is original research papers relating specifically to neuroscience and was established in May 1998. According to the Journal Citation Reports, Nature Neuroscience had a 2016 impact factor of 17.839.

Overdeepening

Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are hundreds of metres below the deepest continuous line (the thalweg) along a valley or watercourse. This phenomenon is observed under modern day glaciers, in salt-water fjords and fresh-water lakes remaining after glaciers melt, as well as in tunnel valleys which are partially or totally filled with sediment. When the channel produced by a glacier is filled with debris, the subsurface geomorphic structure is found to be erosionally cut into bedrock and subsequently filled by sediments. These overdeepened cuts into bedrock structures can reach a depth of several hundred metres below the valley floor.Overdeepened fjords and lakes have significant economic value as harbours and fisheries. Overdeepened basins and valleys filled with sediment (termed tunnel valleys) are of particular interest to engineers, petroleum geologists, and hydrologists; engineers apply the information for developing foundations and tunnel construction, petroleum geologists use tunnel valley locations to identify potential oil fields, while hydrologists apply this knowledge for groundwater resource management.

Pull-apart basin

In geology, a basin is a region where subsidence generates accommodation space for the deposition of sediments. A pull-apart basin is a structural basin where two overlapping (en echelon) faults or a fault bend creates an area of crustal extension undergoing tension, which causes the basin to sink down. Frequently, the basins are rhombic or sigmoidal in shape. Dimensionally, basins are limited to the distance between the faults and the length of overlap. Pull-apart basins are also referred to as overlapping-tension-zones (OTZ).

Seasonal flows on warm Martian slopes

Seasonal flows on warm Martian slopes (also called recurring slope lineae, recurrent slope lineae and RSL) are thought to be salty water flows occurring during the warmest months on Mars, or alternatively, dry grains that "flow" downslope of at least 27 degrees.

The flows are narrow (0.5 to 5 meters) and exhibit relatively dark markings on steep (25° to 40°) slopes, appear and incrementally grow during warm seasons and fade in cold seasons. Liquid brines near the surface have been proposed to explain this activity, or dry granular flows. On October 5, 2015, possible RSL were reported on Mount Sharp near the Curiosity rover.

Tor.com

Tor.com is an online science fiction and fantasy magazine published by Tor Books, as well as an imprint of Tor Books.

William Sager

William W. Sager (born August 22, 1954, in Washington, DC) is a marine geophysicist from the University of Houston. Before joining the Houston faculty in 2013, he held the Jane and R. Ken Williams ’45 Chair in Ocean Drilling Science at Texas A&M University from 2003 to 2012.He is best known for his discovery of Tamu Massif—the largest volcano on Earth. Sager began studying Tamu Massif near the end of the 1990s at the Texas A&M College of Geosciences. He and his team published their findings in the September 2013 issue of Nature Geoscience.Sager did his undergraduate studies in physics at Duke University, graduating magna cum laude in 1976. He went on to graduate studies at the University of Hawaii, finishing his doctorate in marine geophysics in 1983. In the same year, he joined the Texas A&M faculty as an assistant professor.

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