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The Southern Hemisphere westerly winds affect the exchange of carbon dioxide between the ocean and atmosphere. Climate reconstructions from the southern mid-latitudes may reveal variability in the strength and position of the wind belt since the Last Glacial Maximum.
Passive margins were thought to be tectonically inactive. Documentation of a volcanic dyke intrusion along the eastern flank of the Red Sea rift proves this plate tectonic tenet wrong, however, with implications for hazard assessments in these regions.
Shifts in the position and intensity of the southern westerly winds recorded at single sites have been suggested to reflect uniform variation throughout the wind belt. Sedimentological analyses from the Andes suggest that changes in the intensity of the winds in the core and northern margin of the westerlies were antiphased during the Holocene epoch.
Large earthquakes are known to trigger subsequent earthquakes in nearby regions, but similar triggering has not been confirmed for volcanic hazards. Analysis of the progressive deformation associated with 13 volcanic dykes intruded in Ethiopia between 2005 and 2009 indicates that magmatic intrusions can help to trigger subsequent intrusions.
Above the 410-km discontinuity in the upper mantle, an intermittent layer characterized by low seismic-wave velocities is thought to represent partial melting in areas of subduction or mantle-plume activity. Seismic data now show that the low-velocity layer extends globally with no affinity to a particular tectonic environment.
The geographic extent of cooling associated with the Antarctic Cold Reversal is unclear. Dating of glacial moraines in New Zealand suggests that the cooling extended into the southern mid-latitudes, possibly as a result of the northward migration of the southern subtropical front.
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.
Volcanic fields at the eastern margin of the Red Sea rift were regarded as seismically quiet until a swarm of 30,000 earthquakes struck in 2009. Geological analyses reveal the intrusion of a volcanic dyke and indicate that rift-related extension is spread over a broad region far from the rift axis.
The Atlantic meridional overturning circulation delivers warmth to high latitudes and carbon to depth. Historical temperature and salinity records call into question the traditional view that these waters form a single coherent conveyer system of currents.
How groundwater flow varies when long-term external conditions change is little documented. Geochemical evidence shows that sea-level rise at the end of the last glacial period led to a shift in the flow patterns of coastal groundwater beneath Florida.
Instrumental records, proxy data and climate modelling show that multidecadal variability is a dominant feature of North Atlantic sea-surface temperature variations. Simulations with a coupled climate model suggest that the timing of this variability is determined mainly by external forcing, for example from volcanic eruption or solar forcing.
Sea-level fluctuations can have a profound impact on coastal groundwater circulation. The geochemistry of groundwater in the Floridan aquifer system suggests that the fresh water in the upper aquifer was emplaced primarily during the last glacial period, when sea level was more than 100 m lower than at present.
Hydrographic properties of the North Atlantic Ocean have changed significantly over the past decades. A combination of changes in seawater density, calculated from observed properties of sea water and a numerical ocean model, reveals that the strength of the meridional overturning circulation has changed in different directions in the subpolar and subtropical basins, respectively.
European heatwaves have raised interest in the impact of land-cover conditions on temperature extremes. Analyses of observations from an extensive network of flux towers in Europe reveal a difference in the response of forests and grassland to extreme or long-lasting heat.
