The following highlights summarize research papers that have been recently published in Geophysical Research Letters (GRL), Journal of Geophysical Research-Atmospheres (JGR-D), and Journal of Geophysical Research-Solid Earth (JGR-B).
In this release:
- Measuring mercury in coastal fog water
- Early Eocene climate warming increased petroleum production
- Unexpected earthquakes within continental plates pose challenges
- Land use changes contribute to climate extremes
- When will warming-induced rainfall changes be perceptible?
- Model describes New Zealand's complex tectonic environment
- Geomagnetic data reveal unusual nature of recent solar minimum
Anyone may read the scientific abstract for any already-published paper by clicking on the link provided at the end of each Highlight. You can also read the abstract by going to http://www.agu.org/pubs/search_options.shtml and inserting into the search engine the full doi (digital object identifier), e.g. 10.1029/2011GL050324. The doi is found at the end of each Highlight below.
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1. Measuring mercury in coastal fog water
Mercury, a heavy metal neurotoxin, accumulates in sea life, in some cases reaching levels that make seafood unsafe for humans to eat. How mercury gets into aquatic organisms is debated, but part of the pathway could include mercury carried in precipitation, including rain, snow, and fog. The contribution of mercury in fog water in particular is not well known, especially in foggy coastal areas such as coastal California. To learn more, Weiss-Penzias et al. measured total mercury and monomethyl mercury concentrations in fog water and rainwater samples taken from four locations around Monterey Bay, California, during spring and summer 2011. They find that the mean monomethyl mercury concentrations in their fog water samples are about 34 times higher than the mean concentrations in their rainwater samples. Therefore, the authors believe that fog is an important, and previously unrecognized, source of mercury to coastal ecosystems. They also explored potential sources of mercury, finding that biotically formed monomethyl mercury from oceanic upwelling may contribute to monomethyl mercury in fog.
Geophysical Research Letters, doi:10.1029/2011GL050324, 2012
Title: Total and monomethyl mercury in fog water from the central California coast
Authors: Peter S. Weiss-Penzias, Cruz Ortiz Jr., and R. Paul Acosta: Department of Microbiology and Environmental Toxicology, University of California, Santa Cruz, California, USA;
Wesley Heim: Moss Landing Marine Laboratory, California State University, Moss Landing, California, USA;
John P. Ryan: Monterey Bay Aquarium Research Institute, Moss Landing, California, USA;
Daniel Fernandez: Division of Science and Environmental Policy, California State University, Monterey Bay, Seaside, California, USA;
Jeffrey L. Collett Jr.: Department of Atmospheric Science, Colorado State University, Fort Collins, Colorado, USA;
A. Russell Flegal: Department of Microbiology and Environmental Toxicology, University of California, Santa Cruz, California, USA.
2. Early Eocene climate warming increased petroleum production
From the late Paleocene, about 58 million years ago, to the early Eocene, about 51 million years ago, Earth's surface temperatures warmed by about 5-10 degrees Celsius (9 to 18 degrees Fahrenheit). Also in the early Eocene, there was an increase of carbon-13-depleted carbon in the oceans that cannot be accounted for by changes in carbon cycling at the surface. To better understand the source of that carbon, Kroeger and Funnell modeled the thermal evolution of four sedimentary basins in the southwestern Pacific Ocean. They show that the rising surface temperatures of the early Eocene eventually led to warming of the sedimentary beds deep beneath the surface. Petroleum can be produced at only a certain range of temperatures; the rising temperatures at greater depths would have brought more potential source rocks into temperature conditions under which oil and gas can be produced and released. In fact, the researchers find that the early Eocene warming would have led to the production and release of 50 percent more oil and gas than would have occurred under a constant temperature scenario. Some of this newly produced oil and gas would not have been trapped in sedimentary layers deep in the basin but would have leaked to the surface and potentially reached the atmosphere, where it could have acted as a climate feedback, causing further warming.
Geophysical Research Letters, doi:10.1029/2011GL050345, 2012
Title: Warm Eocene climate enhanced petroleum generation from Cretaceous source rocks: A potential climate feedback mechanism?
Authors: K. F. Kroeger and R. H. Funnell: Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand.
3. Unexpected earthquakes within continental plates pose challenges
Earthquakes that occur on "passive" continental margins, such as the August 2011 magnitude 5.8 Mineral, Virginia, earthquake, surprise people because they expect earthquakes to occur only on plate boundaries. But, in fact, large and damaging intraplate earthquakes occur fairly regularly on passive margins around the world. For instance, in North America the approximately magnitude 7 Charleston earthquake shook South Carolina in 1886, causing severe damage and about 60 deaths, and the 1929 magnitude 7.2 earthquake on the Grand Banks of Newfoundland, Canada, caused a tsunami, a large landslide, and 28 fatalities.
Although they are fairly common, these earthquakes are not well studied, and their specific geologic settings and causes are unclear. Wolin et al. review what is known about these earthquakes and describe some of the challenges. They note that these quakes, which occur both onshore and offshore, are thought to be caused by reactivation of ancient faults created by previous continental collision and breakup. Stresses causing passive margin earthquakes could be due to plate- wide forces, glacial isostatic adjustment, local stresses, or other factors, but no comprehensive model explains all of these earthquakes. Aftershocks of passive margin earthquakes can occur for hundreds of years.
One challenge is that because large intraplate events occur infrequently and small events are not well recorded, it has been difficult for scientists to collect enough data on passive margin quakes to form a complete understanding. However, GPS is making it possible to track tiny crustal deformations as small as one millimeter per year (0.038 inches per year), so scientists can identify areas where strain is building. The authors conclude that it is important to continue research on these quakes, integrating seismic, geodetic, and geological techniques, to learn more about the mechanisms causing passive margin earthquakes and to improve hazard assessment.
Geophysical Research Letters, doi:10.1029/2011GL050310, 2012
Title: Mineral, Virginia, earthquake illustrates seismicity of a passive-aggressive margin
Authors: Emily Wolin and Seth Stein: Department of Earth and Planetary Sciences, Northwestern University, Evanston, Illinois, USA;
Frank Pazzaglia and Anne Meltzer: Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania, USA;
Alan Kafka: Weston Observatory, Department of Earth and Environmental Sciences, Boston College, Weston, Massachusetts, USA;
Claudio Berti: Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania, USA.
4. Land use changes contribute to climate extremes
Temperature extremes such as severe heat waves and cold spells are likely to occur more frequently in a warming climate as carbon dioxide (CO2) concentrations rise. But land use change, such as clearing forests for agriculture, also has a large impact on extreme temperature events. To determine the relative contribution of the two effects, Avila et al. ran simulations using a climate model coupled to a sophisticated land surface model. They find that land use changes can have a significant effect on temperature extreme indices. On regional scales, land use changes in some cases amplified the effects of increased CO- 2 concentrations, while land use changes in other cases masked their effects. In some regions, the effects of land use changes on temperature extremes were similar in magnitude to those of doubling CO2. They conclude that land use changes are a major source of human influence on the climate.
Journal of Geophysical Research-Atmospheres, doi:10.1029/2011JD016382,
Title: Climate model simulated changes in temperature extremes due to land cover change
Authors: F. B. Avila, A. J. Pitman, M. G. Donat, L. V. Alexander, and G. Abramowitz: Climate Change Research Centre, University of New South Wales, Sydney, New South Wales, Australia.
5. When will warming-induced rainfall changes be perceptible?
Global climate change is not only changing temperatures but also altering precipitation. These changes in precipitation have been studied on large regional levels, but studies have not been able to identify changes in observed precipitation on smaller spatial scales. Natural interannual variability also makes it difficult to perceive precipitation changes caused by global warming at a statistically significant level. Using general circulation climate models to study future precipitation changes, Mahlstein et al. estimated by how much global temperatures would need to increase for the warming-induced precipitation changes to be clearly noticeable on local or regional scales. They find that temperatures would need to be 1.4 degrees Celsius (2.5 degrees Fahrenheit) warmer than they were in the early twentieth century for regional precipitation changes to be statistically significant. The authors note that this is likely to occur by the end of this century.
Geophysical Research Letters, doi:10.1029/2011GL050738, 2012
Title: Perceptible changes in regional precipitation in a future climate
Authors: Irina Mahlstein, Robert W. Portmann, and John S. Daniel: Earth System Research Laboratory, NOAA, Boulder, Colorado, USA;
Susan Solomon: Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, Colorado, USA and Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA;
Reto Knutti: Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland.
6. Model describes New Zealand's complex tectonic environment
At the Hikurangi fault, off the eastern coast of New Zealand's North Island, the Pacific tectonic plate sinks beneath the Australian plate. Farther south, in the Marlborough Fault System, which cuts through the country's larger South Island, the interaction between the two slabs turns such that the plates grind edge-on. From north to south, over a relatively short length of the plate boundary, the interaction switches from subduction to strike-slip. Though the fault systems near each of New Zealand's major islands have been studied extensively, the intervening region that harbors the transition between the two modes of interaction is much less well understood. Exploring the subduction-to-strike-slip transition region could help explain how and whether the fault systems that populate the country are connected and potentially improve estimates of seismic risk.
Seeking to fill out the picture of New Zealand's tectonic environment, Wallace et al. modeled the independent fragments of the Earth's crust that make up the larger plate boundary. Using measurements of known fault locations and stresses, combined with recordings of ground velocity measurements drawn from 800 GPS ground stations distributed across the country, the authors reverse engineered the complex system of faults that crosses New Zealand. The authors find that the switch from subduction in the north to strike-slip in the south is due to what they describe as a kink in the Australian plate that cuts across the northern South Island. They suggest that this deformation acts as a hinge about which the northern part of the Pacific plate takes on a clockwise rotation. Further, the authors' model allowed them to estimate the slip rate deficit for each fault, a measure of the expected but as of yet unobserved plate motion that could indicate an ongoing buildup of energy within the fault.
Journal of Geophysical Research-Solid Earth, doi:10.1029/2011JB008640, 2012
Title: The kinematics of a transition from subduction to strike-slip: An example from the central New Zealand plate boundary
Authors: L. M. Wallace, J. Beavan, R. Van Dissen, N. Litchfield, R. Langridge, and N. Pondard: GNS Science, Lower Hutt, New Zealand;
P. Barnes, J. Mountjoy, and G. Lamarche: National Institute of Water and Atmospheric Research, Wellington, New Zealand.
7. Geomagnetic data reveal unusual nature of recent solar minimum
Since the mid-1800s, scientists have been systematically measuring changes in the Earth's magnetic field and the occurrence of geomagnetic activity. Such long- term investigation has uncovered a number of cyclical changes, including a signal associated with 27-day solar rotation. This is most clearly seen during the declining phase and minimum of each 11-year solar cycle, when the Sun's magnetic dipole is sometimes tilted with respect to the Sun's rotational axis. With the Sun's rotation and the emission of solar wind along field lines from either end of the solar magnetic dipole, an outward propagating spiral-like pattern is formed in the solar wind and the interplanetary magnetic field that can drive 27-day, and occasionally 13.5-day, recurrent geomagnetic activity. Recurrent geomagnetic activity can also be driven by isolated and semipersistent coronal holes, from which concentrated streams of solar wind can be emitted.
During the most recent solar minimum, which took place from 2006 to 2010, however, several researcher groups noticed 6.7-day and 9-day recurrent changes in geomagnetic activity, and similar patterns in the interplanetary magnetic field, and the solar wind. Using modern data covering the previous two solar minima, these higher-frequency occurrences were judged to be unusual. Love et al. analyzed historical geomagnetic activity records from 1868 to 2011 and find that the 6.7-day and 9-day recurrent changes were actually unique in the past 140 years. They suggest that the higher-frequency changes in geomagnetic activity are due to an unusual transient asymmetry in the solar dynamo, the turbulent, rotating plasma deep within the sun which generates the magnetic field.
Geophysical Research Letters, doi:10.1029/2011GL050702, 2012
Title: Geomagnetic detection of the sectorial solar magnetic field and the historical peculiarity of minimum 23-24
Authors: Jeffrey J. Love and E. Joshua Rigler: Geomagnetism Program, U.S. Geological Survey, Denver, Colorado, USA;
Sarah E. Gibson: High Altitude Observatory, NCAR, Boulder, Colorado, USA.