- Issue
Geophysical Research Letters: Volume 40, Issue 11
2479-287716 June 2013
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Regular Articles
Space Sciences
Saturn's magnetospheric refresh rate
- Pages: 2479-2483
- First Published: 03 May 2013
- Saturn has a magnetospheric frequency close to the planet's rotation rate
- We confirm that Jupiter's natural refresh rate is 2-3 days
- This result is relevant to the ongoing mystery of periodic phenomena at Saturn
SAMI3 simulation of plasmasphere refilling
- Pages: 2484-2488
- First Published: 11 April 2013
- Refilling is simulated with E x B drifts in all three dimensions
- Because of corotation, diurnal variations are strong at fixed local time
- The quiet-time plasmasphere morphology repeats daily
Field-aligned current reconfiguration and magnetospheric response to an impulse in the interplanetary magnetic field BY component
- Pages: 2489-2494
- First Published: 25 April 2013
- An impulse in IMF By drives fast flows in the high latitude ionosphere
- The peak dawn-side FAC strength occurs 1.25 hours after the impulse
- The FAC strength correlates well with solar wind MA and SYM-H
An indication of the existence of a solar wind strahl at 10 AU
- Pages: 2495-2499
- First Published: 03 May 2013
- First observations of suprathermal solar wind electrons outside 5AU
- Unexpected presence of a distinct strahl component to the distribution
- This implies pitch angle scattering rates decrease with heliocentric distance
Dynamics and distribution of nano-dust particles in the inner solar system
- Pages: 2500-2504
- First Published: 06 May 2013
- The acceleration of nano-dust to near solar wind speed is calculated
- The intermittent nature of the observations can be due to the IMF configuration
- Observations do not allow conclusions about the origin of these particles
Oscillatory flow braking in the magnetotail: THEMIS statistics
- Pages: 2505-2510
- First Published: 25 March 2013
- Damped oscillatory flow in the plasma sheet is caused by oscillating flux tube
- Oscillation period can be reliably estimated using MHD theory
- Group parameters of the damped oscillatory flows are given
Observation of multiple sub-cavities adjacent to single separatrix
- Pages: 2511-2517
- First Published: 07 May 2013
- Multiple sub-cavities adjacent to the separatrix
- Electron acceleration in the separatrix
- Unipolar parallel and oscillating perpendicular electric field in the separatrix
Discriminating the tectonic and non-tectonic contributions in the ionospheric signature of the 2011, Mw7.1, dip-slip Van earthquake, Eastern Turkey
- Pages: 2518-2522
- First Published: 10 May 2013
- New near-source coseismic ionospheric observations using GPS and GLONASS
- Signals carry information on the seismic rupture slip mode
- Initial polarity and amplitude distributions explained using a full 3D modeling
Longitudinal and day-to-day variability in the ionosphere from lower atmosphere tidal forcing
- Pages: 2523-2528
- First Published: 13 May 2013
- Ionospheric variability is simulated by a coupled atmosphere-ionosphere model
- Ionospheric longitudinal variations are driven by the non-migrating tides
- Lower atmosphere tidal forcing can cause about half of the diurnal variability
Planets
Intensities of the Martian N2 electron-impact excited dayglow emissions
- Pages: 2529-2533
- First Published: 01 April 2013
- We have computed the intensities of 15 band systems of N2 on Mars
- The intensities of the VK emissions agree with SPICAM limb profiles
- Our calculations do not require that the mixing ratio of N2 be reduced
Does folding accommodate Europa's contractional strain? The effect of surface temperature on fold formation in ice lithospheres
- Pages: 2534-2538
- First Published: 01 May 2013
- Fold growth rates are a strong function of surface temperature
- Folding requires larger strains at Europan equatorial temperatures
- Passive shortening during contraction helps explain Europa's strain imbalance
Limb imaging of the Venus O2 visible nightglow with the Venus Monitoring Camera
- Pages: 2539-2543
- First Published: 14 May 2013
- The Venus O2 visible nightglow is investigated for over 4 years with VMC
- The O2 visible nightglow is brighter near the equator and faints polewards
- The evidence from VMC and VIRTIS suggests that the two emissions correlate
Solid Earth
Electrical resistivity tomography revealing the internal structure of monogenetic volcanoes
- Pages: 2544-2549
- First Published: 08 May 2013
- Electrical resistivity tomography was performed on monogenetic volcanoes
- The eruptive conduit of a Strombolian cone was identified
- ERT imaging contributes in volcanic forecasting by the identification of hazards
Arc magma compositions controlled by linked thermal and chemical gradients above the subducting slab
- Pages: 2550-2556
- First Published: 29 April 2013
- Mafic arc rocks preserve a systematic down-slab magma chemical gradient
- This reflects increasing dominance of hydrous melts in the slab flux
- This change, over a few km, is a first-order control on melt chemistry
Observations of core-mantle boundary Stoneley modes
- Pages: 2557-2561
- First Published: 01 May 2013
- We present CMB Stoneley mode splitting function measurements
- The CMB Stoneley mode splitting correlates well with diffracted body wave data
- Our measurements allow to constrain density variations in the lowermost mantle
The 2011 M = 9.0 Tohoku oki earthquake more than doubled the probability of large shocks beneath Tokyo
- Pages: 2562-2566
- First Published: 02 May 2013
- Tokyo seismicity rate jumped 10-fold even though the M9 shock struck 200 km away
- The data can be explained by stress triggering, permitting a 5-yr M>7 forecast
- Capturing highly time-dependent hazard is critical to megacities near megaquakes
Monitoring deformation at the Geysers Geothermal Field, California using C-band and X-band interferometric synthetic aperture radar
- Pages: 2567-2572
- First Published: 07 March 2013
- X-band data provides improved coverage of deformation at The Geysers
- The C-band deformation rate agrees with past estimates
- The estimates are supported by modeling
Using hydroacoustic stations as water column seismometers
- Pages: 2573-2578
- First Published: 21 March 2013
- We show how to convert pressure data to vector seismic data
Constraints on the composition of the Aleutian arc lower crust from VP/VS
- Pages: 2579-2584
- First Published: 20 March 2013
- VP/VS ratio estimated for Aleutian lower crust from along-arc refraction line
- Results indicate abundant clinopyroxenite, consistent with geochemistry
- Alpha quartz is an important control on crustal velocities in arcs
Convergence of the frequency-size distribution of global earthquakes
- Pages: 2585-2589
- First Published: 28 March 2013
- The tail of the global frequency-magnitude distribution is poorly constrained
- Convergence properties are inconsistent with an unbounded GR distribution
- The global catalogue is a mix of superposed randomly-sampled regional catalogues
Linking permeability to crack density evolution in thermally stressed rocks under cyclic loading
- Pages: 2590-2595
- First Published: 02 April 2013
- Identification of 3 regimes of permeability approaching failure
- Identification of the role of cooling rates on crack geometry and connectivity
- Prediction of the coupled permeability and microcrack network evolution
Stress tensor changes related to fluid injection at The Geysers geothermal field, California
- Pages: 2596-2601
- First Published: 03 April 2013
- Fluid injection causes local temporal variations of the stress field orientation
- Long-term fluid extraction results in changes of the stress regime with depth
- Stress inversion applied to microseismicity improves reservoir characterization
California foreshock sequences suggest aseismic triggering process
- Pages: 2602-2607
- First Published: 03 April 2013
- Foreshocks are triggered by aseismic process which may trigger the mainshocks
- Foreshocks are less energetic than aftershock and background seismicity
- The stress drop history suggests similarity between foreshocks and swarms
Active blind thrusts beneath the Tokyo metropolitan area: Seismic hazards and inversion tectonics
- Pages: 2608-2612
- First Published: 19 April 2013
- Blind thrust structures in Tokyo were imaged in deep seismic profiles
- Fault activity was estimated by shallow seismic profile and borehole transect
- Low slip rates pose a problem on infrequent but devastating seismic hazards
Characterization of fluid flow in a shear band in porous rock using neutron radiography
- Pages: 2613-2618
- First Published: 03 May 2013
- Fluid flow into sandstone is tracked by neutron radiography and image analyses
- Measurements of local water imbibition rates are made in a shear band
- Comparison is made of flow and 3D strain fields (from digital image correlation)
Effects of pore fluid pressure on slip behaviors: An experimental study
- Pages: 2619-2624
- First Published: 09 May 2013
- A new experimental setup is designed to investigate pore pressure effect on slip
- Excess pore pressure can induce slip instability on an otherwise creeping fault
- Deformation mechanisms that control such different behaviors are identified
Rapid ice melting drives Earth's pole to the east
- Pages: 2625-2630
- First Published: 13 May 2013
- First explained the abrupt departure of the mean pole position in recent years.
- Polar motion provides constraints to study of ice melting and sea level rise.
- Polar motion is useful in bridging the gap between GRACE and follow-on missions.
Assessing the potential improvement in short-term earthquake forecasts from incorporation of GPS data
- Pages: 2631-2635
- First Published: 14 May 2013
- Anomalies in GPS data are extracted and show short-term precursory information
- These GPS signals are not caused by the earthquakes
- GPS data can be used to augment probability models for earthquake forecasting
Azimuthal anisotropy at Valhall: The Helmholtz equation approach
- Pages: 2636-2641
- First Published: 06 April 2013
- Seismic interferometry is applied to passive data from an industrial network
- 6 hours of data are sufficient to measure seismic anisotropy
- We demonstrate that the azimuthal anisotropy is dominated by the 2psi term
The role of hydrous phases in the formation of trench parallel anisotropy: Evidence from Rayleigh waves in Cascadia
- Pages: 2642-2646
- First Published: 02 May 2013
- Cascadia exhibits trench parallel anisotropy in Rayleigh wave phase velocities
- Rayleigh wave depth constraints show this anisotropy at 50 -110 km depth
- Most likely cause is the presence of hydrous phases in or just above the slab
Effects of continental configuration on mantle heat loss
- Pages: 2647-2651
- First Published: 09 May 2013
- When distributed, continents can cause flow patterns to become locked
- Continents can impose long-term thermal structures mimicking a thermal plume
- An Earth with >50% continents would not possess plate tectonics
Implications of high core thermal conductivity on Earth's coupled mantle and core evolution
- Pages: 2652-2656
- First Published: 20 May 2013
- We assess the thermal and magnetic evolution of Earth's core
- T-C structures in the mantle are identical with various core properties
- Extremely high thermal conductivity causes a 100s km of sub-adiabatic region
A new way to detect volcanic plumes
- Pages: 2657-2660
- First Published: 14 May 2013
- Detection of plumes is of interest for both geophysics and aircraft safety
- Plumes are detectable in real-time with GPS
- This method isn't influenced by position changes
Low-frequency earthquakes in the Mexican Sweet Spot
- Pages: 2661-2666
- First Published: 16 May 2013
- Detected and characterized 15 low-frequency earthquake families in Mexico
- Sources locate to a region known for constant non-volcanic tremor activity
- Focal mechanisms reflect shearing on the subducting plate interface
Hydrology and Land Surface Studies
Paleofire reconstruction based on an ensemble-member strategy applied to sedimentary charcoal
- Pages: 2667-2672
- First Published: 25 April 2013
- Our innovative approach enables to determine robust fire event dates
- We assessed paleofire frequency using ensemble member's reconstructions
Quantifying the modern recharge of the “fossil” Sahara aquifers
- Pages: 2673-2678
- First Published: 17 April 2013
- Sahara aquifers are recharged at present-day with a renewal rate of 40%
- Infiltration towards the water table takes at least 9 to 12 month
- Groundwater budget involving GRACE is a relevant approach in semiarid regions
Cryosphere
Energy budget of first-year Arctic sea ice in advanced stages of melt
- Pages: 2679-2683
- First Published: 02 May 2013
- First-year sea ice reflects less and transmits more sunlight than multiyear ice
- The increased transmittance allows for greater ocean heat fluxes
- Some transmitted energy is stored, released later in the year or during storms
Recent snowfall anomalies in Dronning Maud Land, East Antarctica, in a historical and future climate perspective
- Pages: 2684-2688
- First Published: 15 May 2013
- Recent East Antarctic snowfall anomalies are unparalleled since 1979
- Firn core data suggest that there have been similar anomalies before the 1950's
- Such anomalies are projected to occur more frequently in future
High biolability of ancient permafrost carbon upon thaw
- Pages: 2689-2693
- First Published: 15 March 2013
- Ancient dissolved OC (>21ky) is mobilized in thaw streams draining Yedoma cliffs
- The dissolved OC is highly biolabile: 34+/-1% was lost during 14-d incubations
- Yedoma OC reactivity should be incorporated in regional and global C budgets
Modeling the influence of photochemistry on hydrogen peroxide concentrations in an Arctic snowpack
- Pages: 2694-2698
- First Published: 27 May 2013
- We modeled one year of hydrogen peroxide photochemistry in a polar snowpack
- Photolysis can destroy up to 40% of HOOH deposited in summer
- Photochemistry complements physical mechanisms to control HOOH concentrations
Correction
Cryosphere
Correction to “Changes in Arctic sea ice result in increasing light transmittance and absorption”
- Pages: 2699-2700
- First Published: 02 May 2013
Regular Articles
Oceans
Climate-driven sea level anomalies modulate coastal groundwater dynamics and discharge
- Pages: 2701-2706
- First Published: 26 January 2013
- Salinity of the coastal aquifer mixing zone is dynamic across a 4 year time series
- Mean sea level oscillations drive the coastal hydraulic gradient
- Coastal aquifer geochemistry is sensitive to climate-influenced sea level anomalies
Tidal dissipation in the early Eocene and implications for ocean mixing
- Pages: 2707-2713
- First Published: 26 April 2013
- The tidal dissipation during the Eocene was weaker than at present
- The abyssal Pacific was the main location of tidal dissipation
- The vertical mixing in the Eocene Pacific was stronger than at present
Interaction network based early warning indicators for the Atlantic MOC collapse
- Pages: 2714-2719
- First Published: 01 May 2013
- New indicators for MOC collapse
- Indicators based on spatial correlations
- Network analysis useful to monitor critical transitions
Aragonite saturation state dynamics in a coastal upwelling zone
- Pages: 2720-2725
- First Published: 11 April 2013
- Aragonite saturation states are calculated from time series pH and pCO2 data
- Seasonal processes controlling aragonite saturation state are determined
- Current coastal upwelling zone variability compared to preindustrial range
A mechanism for sandbar straightening by oblique wave incidence
- Pages: 2726-2730
- First Published: 12 April 2013
- We show why oblique waves induce morphological reset of surf-zone rhythmic bars
- Rip currents are weakened and shifted alongshore for increasing wave obliquity
- Crescentic bar straightening is highly sensitive to the offshore wave angle
Shipping contributes to ocean acidification
- Pages: 2731-2736
- First Published: 01 May 2013
- Ocean acidification attributable to shipping emissions deposition is modeled
- Ship-derived acidification in heavily trafficked areas can equal that from CO2
- Future ship sulfur reductions create a natural geophysical experiment
Intraseasonal variations in the surface layer heat balance of the central equatorial Indian Ocean: The importance of zonal advection and vertical mixing
- Pages: 2737-2741
- First Published: 06 May 2013
- Two MJO events forced an SST decrease that was in part due to reduced heat flux
- For one MJO zonal advection contributed substantial cooling
- For other event lack of barrier layer enabled pronounced entrainment
Eddy-induced variability of the meridional overturning circulation in a model of the North Atlantic
- Pages: 2742-2747
- First Published: 06 May 2013
- Unpredictable eddy-induced overturning variability is isolated in 1/10deg model
- Eddies make up 2/3 of overturning variability in the subtropics and 1/3 outside
- An important component of eddy driven overturning is at interannual time scales
Large-amplitude internal tides, solitary waves, and turbulence in the central Bay of Biscay
- Pages: 2748-2754
- First Published: 06 May 2013
- Internal tides and solitary waves are characterized in the central Bay of Biscay
- Microstructure measurements are firstly presented in the central Bay of Biscay
- Observed dissipation rates are reproduced by the Mackinnon-Gregg scaling
Remotely induced warming of Antarctic Bottom Water in the eastern Weddell gyre
- Pages: 2755-2760
- First Published: 02 May 2013
- Bottom Water from Cape Darnley, Antarctica has warmed and lightened 1993-2008
- Warming linked to changes in mixing with the Circumpolar Current
- This new mechanism may affect other regions of the Southern Ocean
The response of the large-scale ocean circulation to 20th century Asian and non-Asian aerosols
- Pages: 2761-2767
- First Published: 28 May 2013
- Anthropogenic aerosols force circulation changes to the global ocean
- Non-Asian aerosols account for most of the aerosol-induced circulation trends
- As non-Asian sulfate aerosols peaked in the 1980s, the trends may be reversing
Climate
Uncertainty in future regional sea level rise due to internal climate variability
- Pages: 2768-2772
- First Published: 03 May 2013
- Internal climate variability can affect the regional sea level
- Regional sea level rise can significantly differ from the global mean changes
- Ocean dynamics plays important role on regional sea level rise
Decadal prediction of observed and simulated sea surface temperatures
- Pages: 2773-2778
- First Published: 25 January 2013
- This paper shows that SSTs can be predicted with skill on decadal time scales
- Patterns of SST that can be predicted are identified explicitly
- Initial condition information improves climate predictions
Spatiotemporal distribution patterns of dissolved methane in lakes: How accurate are the current estimations of the diffusive flux path?
- Pages: 2779-2784
- First Published: 12 April 2013
- In lakes, bays and extended littoral zones are
- Dissolved methane and diffusive efflux are heterogeneously distributed
- Heterogeneous distributions of methane affect the accuracy flux estimations
The climate impact of aviation aerosols
- Pages: 2785-2789
- First Published: 01 May 2013
- Aviation Aerosol Impacts affect liquid clouds below flight levels
- Effect is mostly a cooling due to SO4 emissions
- Cooling is larger than expected warming from contrails
Variability of central United States April–May tornado day likelihood by phase of the Madden-Julian Oscillation
- Pages: 2790-2795
- First Published: 02 May 2013
- Relationship between MJO and central U.S. tornado days examined
- Environmental parameters explain tornado day anomalies
- Implications for extended range forecasting of central U.S. tornado days
Climate impact of stratospheric ozone recovery
- Pages: 2796-2800
- First Published: 14 March 2013
- climate impact of stratospheric ozone recovery
Revisiting the controversial issue of tropical tropospheric temperature trends
- Pages: 2801-2806
- First Published: 15 April 2013
- High horizontal resolution models improve temperature trends
- There is no discrepancy in tropical temperature trends
- Observational uncertainty needs to be considered
Decadal predictability of tropical basin average and global average sea surface temperatures in CMIP5 experiments with the HadCM3, GFDL-CM2.1, NCAR-CCSM4, and MIROC5 global Earth System Models
- Pages: 2807-2812
- First Published: 12 February 2013
- Estimate of decadal hindcast skill of sea surface temperature anomalies
- Hindcast experiments with four Global Earth System Models from 1960 to 2010
- Significant skill in some ocean basin-decade combinations
Atmospheric Science
Recent observations of high mass density polar mesospheric clouds: A link to space traffic?
- Pages: 2813-2817
- First Published: 08 May 2013
- No solar cycle variation in polar mesospheric clouds
- Meteorological variation and rocket exhaust dominate cloud occurrence
- Enhanced mesospheric water vapor in 2011 and 2012
GNSS observations of deep convective time scales in the Amazon
- Pages: 2818-2823
- First Published: 20 May 2013
- A new timescale is developed for the shallow-to-deep convective transition
- First ever, long-term study of deep convection in the tropics using GNSS/GPS
- Convergence timescale is robust, independent of forcing/nature of the convection
On the parameterization of surface momentum transport via drag coefficient in low-wind conditions
- Pages: 2824-2828
- First Published: 01 May 2013
- Surface layer momentum transport is investigated using 20Hz tower data
- Drag coefficient increases with a decrease in wind speed for low wind speeds
- A new parameterization framework for drag coefficient is developed
Interpreting seasonal changes in the carbon balance of southern Amazonia using measurements of XCO2 and chlorophyll fluorescence from GOSAT
- Pages: 2829-2833
- First Published: 08 April 2013
- XCO2 exhibits strong seasonal variability (~ 4 ppm) in southern Amazonia
- This is possible because vertical mixing and local seasonal NEE are coupled
- XCO2 is inversely correlated with fluorescence, indicating GPP drives NEE
Adsorption of organic molecules may explain growth of newly nucleated clusters and new particle formation
- Pages: 2834-2838
- First Published: 12 April 2013
- Organic molecules may adsorb on the surface of nascent clusters
- Adsorption may facilitate the condensation of organics on nascent clusters
- Adsorption of organics may explain enhanced initial particle growth rate
Surface ozone variability and the jet position: Implications for projecting future air quality
- Pages: 2839-2844
- First Published: 27 March 2013
- Ozone variability is a function of the jet position
- Surface ozone variability follows the jet in future climate simulations
- Regional ozone-temperature relationships may change in the future
Anthropogenic sulfate aerosol and the southward shift of tropical precipitation in the late 20th century
- Pages: 2845-2850
- First Published: 24 April 2013
- A southward shift of tropical rain in the 1980s is detected in observations
- Most CMIP3/5 GCMs simulate the shift, although less than observed
- Anthropogenic sulfate emissions cause most of the southward shift in the GCMs
Response of extratropical cyclone activity to the Kuroshio large meander in northern winter
- Pages: 2851-2855
- First Published: 10 May 2013
- High-resolution air-sea coupled model reproduces a large meander of the Kuroshio
- Its meander leads to decreased latent heat flux and weakened baroclinicity
- Primary path of cyclones is very sensitive to the large meander of Kuroshio
A robust mode of climate variability in the Arctic: The Barents Oscillation
- Pages: 2856-2861
- First Published: 16 May 2013
- The Barents Oscillation (BO) is a robust mode of atmospheric variability
- The BO is well related to westerly wind anomalies into the Barents Sea
- Temperature anomalies in the Barents Sea can largely be explained by the BO
Interannual variability of tropical tropopause layer clouds
- Pages: 2862-2866
- First Published: 29 April 2013
- Extreme interannual variability in TTL cloudiness identified with A-train data
- QBO, ENSO, and the Brewer-Dobson circulation impact zonal mean TTL cloudiness
- ENSO causes zonally-asymmetric TTL cloud anomalies
Contrail ice particles in aircraft wakes and their climatic importance
- Pages: 2867-2872
- First Published: 08 May 2013
- Gaseous and ice particle concentrations were measured within aircraft wakes
- Contrails contain more ice particles than expected for previous BC estimates
- Ice particle concentration in contrails is important for aviation climate impact
Toward resolution-independent dust emissions in global models: Impacts on the seasonal and spatial distribution of dust
- Pages: 2873-2877
- First Published: 25 March 2013
- Better representation of sub-grid winds reduces resolution dependence of dust
- Improved dust seasonality and spatial distribution for coarse resolution models
- Sea-salt emissions are found to be relatively independent of model resolution