Research Highlights |
Featured
-
-
Letter |
Broad range of 2050 warming from an observationally constrained large climate model ensemble
The global-mean temperature evolution over the course of the twenty-first century is uncertain. Simulations with an ensemble of thousands of climate models that reproduce observed warming over the past 50 years suggest that a mid-range greenhouse-gas emissions scenario without mitigation could lead to a warming of between 1.4 and 3 K by 2050, relative to 1961–1990.
- Daniel J. Rowlands
- , David J. Frame
- & Myles R. Allen
-
-
Editorial |
Sandblasted by the Sun
The Earth's magnetic field protects us from solar activity, but the Moon and Mars are more exposed. The upcoming solar maximum is the perfect time to observe how our dynamic Sun affects its planets.
-
Letter |
Recent extensional tectonics on the Moon revealed by the Lunar Reconnaissance Orbiter Camera
On the Moon, extensional tectonic features have only been observed close to the influence of the mare basalt-filled basins and floor-fractured craters. Analysis of Lunar Reconnaissance Orbiter Camera images reveals several potentially very young extensional tectonic features in the farside highlands, implying that extensional stresses may locally exceed compressional ones.
- Thomas R. Watters
- , Mark S. Robinson
- & Brett W. Denevi
-
-
Letter |
Two boundary layers in Titan’s lower troposphere inferred from a climate model
Saturn’s moon Titan has a dense atmosphere, but its thermal structure is poorly understood. Simulations with a three-dimensional general circulation model suggest that Titan has a lower atmospheric structure with two boundary layers: a seasonal deep layer, and a shallower one that develops during the course of each day.
- Benjamin Charnay
- & Sébastien Lebonnois
-
-
Letter |
Mesospheric electric breakdown and delayed sprite ignition caused by electron detachment
The electric discharge of a thundercloud in the troposphere is often accompanied by upper-atmospheric electric discharges such as sprites or halos. Numerical simulations of the electric response of the mesosphere to lightning suggest that the process of electron associative detachment is fundamental to upper-atmospheric electrodynamics.
- A. Luque
- & F. J. Gordillo-Vázquez
-
-
Letter |
Equatorial winds on Saturn and the stratospheric oscillation
The stability over time of the zonal jets on the giant planets has been debated. An analysis of observations from the Cassini spacecraft reveals an acceleration of wind velocities in Saturn’s high-altitude equatorial jet between 2004 and 2009, by 20 m s−1 at tropopause level and by 60 m s−1 in the stratosphere.
- Liming Li
- , Xun Jiang
- & Kevin H. Baines
-
-
-
Editorial |
Optimized data logistics
Accessible storage of scientific data is usually mandated, but not often achieved. The task needs people who are interested in information technology and regard it as their primary focus.
-
News & Views |
Water on the Moon
Analysis of the first Apollo samples suggested that Earth's only satellite was bone dry. Spacecraft data and improved analysis techniques now indicate that the Moon is more volatile-rich and complex than previously thought.
- David J. Lawrence
-
Letter |
Cold glacial oceans would have inhibited phyllosilicate sedimentation on early Mars
Phyllosilicate minerals are rare in the Noachian-aged crust of the northern lowlands of Mars, compared with the tropical highlands. Geochemical and climate modelling suggest that this dichotomy is consistent with the presence of a cold ocean fringed by cold-based glaciers.
- Alberto G. Fairén
- , Alfonso F. Davila
- & James F. Kasting
-
News & Views |
Arrow in Titan's sky
An exotic arrow-shaped cloud was discovered in the atmosphere of Saturn's moon Titan last year. Numerical modelling shows how a large-scale atmospheric wave can naturally shape tropical clouds to such an arrow.
- Tetsuya Tokano
-
Letter |
Locally enhanced precipitation organized by planetary-scale waves on Titan
Saturn’s moon Titan exhibits an active weather cycle that involves methane. An analysis of cloud observations and simulations with a general circulation model reveals that convection in Titan’s atmosphere is organized through an interplay of two wave modes, leading to local rates of precipitation of up to twenty times the average.
- Jonathan L. Mitchell
- , Máté Ádámkovics
- & Elizabeth P. Turtle
-
News & Views |
More surprises from the Moon
Volcanic deposits on the Moon are almost entirely composed of basaltic lava flows that make up the dark and extensive mare plains. High-resolution images and compositional data now reveal rare, non-mare volcanism on the Moon's farside.
- Noah Petro
-
Article |
Non-mare silicic volcanism on the lunar farside at Compton–Belkovich
Non-basaltic volcanism is rare on the Moon and has been found predominantly on the lunar nearside. Analysis of Lunar Reconnaissance Orbiter Camera images and spectral data reveal the presence of compositionally evolved, non-basaltic volcanism on the lunar farside.
- Bradley L. Jolliff
- , Sandra A. Wiseman
- & David A. Paige
-
Letter |
Replacement and late formation of atmospheric N2 on undifferentiated Titan by impacts
The origin of Titan’s massive nitrogen atmosphere is largely unknown. Laser-gun experiments and numerical calculations suggest that the nitrogen could have been generated by conversion from ammonia during the period of Late Heavy Bombardment.
- Yasuhito Sekine
- , Hidenori Genda
- & Takafumi Matsui
-
Letter |
Hydrothermal vents as a kinetically stable source of iron-sulphide-bearing nanoparticles to the ocean
Hydrothermal vents emit metals such as iron to the ocean. A chemical analysis of hydrothermal fluids suggests that up to 10% of the iron is present as stable, iron-bearing nanoparticles.
- Mustafa Yücel
- , Amy Gartman
- & George W. Luther III
-
News & Views |
Gathering dust
Chondritic meteorites are remnants of the ancient Solar System. Analysis of the dust rims often found on their constituent particles shows that the rims were swept up while the particles wafted about and collided in a weakly turbulent protoplanetary nebula.
- Jeff Cuzzi
-
Letter |
Earliest rock fabric formed in the Solar System preserved in a chondrule rim
Rock fabrics record the formation, compaction and deformation history of that rock. High-resolution mapping of tiny grains in the Allende CV meteorite reveals preservation of a spherical fabric that may have formed in the solar nebula, and could be the oldest rock fabric to have formed in the Solar System.
- Philip A. Bland
- , Lauren E. Howard
- & Kathryn A. Dyl
-
-
-
Review Article |
The biogeochemical cycle of iron in the ocean
Iron controls phytoplankton growth in large tracts of the global ocean, and thereby influences carbon dioxide drawdown. Recent advances reveal the importance of iron-binding ligands and organic matter remineralization in regulating ocean iron levels.
- P. W. Boyd
- & M. J. Ellwood
-
Letter |
Significant sink of ocean-eddy energy near western boundaries
Ocean eddies generated through instability of the mean flow are a vital component of the energy budget of the global ocean. Modelling combined with satellite altimetry data suggests that the energy from westward-propagating eddies is scattered and eventually dispersed when they reach the western boundary of an ocean basin.
- Xiaoming Zhai
- , Helen L. Johnson
- & David P. Marshall
-
Letter |
Photolytic degradation of methylmercury enhanced by binding to natural organic ligands
Methylmercury is a neurotoxin that accumulates in food webs and poses a significant risk to human health. Laboratory experiments suggest that complexation of methylmercury with sulphur-containing ligands can stimulate its degradation.
- Tong Zhang
- & Heileen Hsu-Kim
-
Research Highlights |
Our choice from the recent literature
-
Letter |
Accelerating uplift in the North Atlantic region as an indicator of ice loss
Vertical motions of the rocky margins of Greenland and Antarctica respond to mass changes of their respective ice sheets, but these motions can be obscured by ancient episodes of glacial advance or retreat. An analysis of the acceleration of vertical motion indicates that accelerated ice loss in western Greenland started in the late 1990s.
- Yan Jiang
- , Timothy H. Dixon
- & Shimon Wdowinski
-
Letter |
Links between eccentricity forcing and the 100,000-year glacial cycle
The 100,000-year glacial cycles are generally thought to be driven by the eccentricity of the Earth’s orbit. Statistical analyses of climate variability and orbital forcing over the past five million years indicate that the glacial cycles are the result of an internal climate oscillation phase locked to the 100,000-year eccentricity cycle.
- Lorraine E. Lisiecki
-
News & Views |
Microplate motion
The fragmentation of continents at convergent plate boundaries is thought to be influenced by the subducting lithosphere. Numerical modelling suggests that instead, the forces exerted by the underlying mantle can drive the formation of continental microplates.
- Christine Siddoway
-
Letter |
Atmospheric nanoparticles formed from heterogeneous reactions of organics
Nanoparticles are a key component of atmospheric aerosols, growing rapidly under ambient conditions. Exposure of nanoparticles to organic vapours shows that various organic species can enhance the growth of nanoparticles.
- Lin Wang
- , Alexei F. Khalizov
- & Renyi Zhang
-
Letter |
Mass-independent fractionation of mercury isotopes in Arctic snow driven by sunlight
In the Arctic spring, sunlight-induced reactions convert gaseous elemental mercury into compounds that are rapidly deposited on the snowpack. Analysis of the isotopic composition of mercury in snow samples collected during an atmospheric mercury depletion event suggests that sunlight triggers the re-emission of mercury from the snowpack.
- Laura S. Sherman
- , Joel D. Blum
- & Thomas A. Douglas