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AGU 2013: Social Science Perspectives on Natural Hazards

American Geophysical Union Fall Meeting - Mon, 12/09/2013 - 14:16

Courtesy Erik http://www.flickr.com/photos/tree_trunks/

 

Are you attending the American Geophysical Union (AGU) meeting this week in San Francisco? Are you interested in hearing from social scientists about Natural Hazards? The Center for Research on Environmental Decisions (CRED) will be there to answer your questions. Below is a schedule of sessions that CRED researchers are speaking at or convening.

We hope to see you there. If you can’t be at AGU in person we encourage you to livestream the sessions here. 

 

Katherine Thompson, CRED PhD candidate, “The Problem with Probability: Why rare hazards feel even rarer”

Thompson_bioTuesday December 10, 1:55-2:10 PM PST, 2000 (Moscone West)
Session: Why Should We Talk About What We Don’t Know? Implications of Communicating Scientific Uncertainty II
How is probability of natural hazards events actually used by decision makers? The presentation will make recommendations on presenting probabilistic information to best take advantage of people’s tendencies to either amplify risk or ignore it, as well as recent findings that may shed light on ways that the negative effects of uncertainty can be mitigated.

 

 

David H. Krantz, CRED co-director, “Coordination of Individual and Organizational Planning for Natural Hazards”
krantz_bioThursday December 12, 1:40-1:55 PM PST, 3002 (Moscone West)
Session: Climate Change Effects on Natural Hazards: Science, Communication and Policy I
Dave Krantz will explore the four different kinds of decision aids needed to improve natural hazard planning: mechanisms that support horizontal dissemination of plans, mechanisms that support vertical dissemination, mechanisms for examining goal conflicts and reducing these through plans that take others’ goals into account, and mechanisms for examining belief conflicts.

 

Poster session, “Climate Change Effects on Natural Hazards: Science, Communication and Policy II Posters 
8:00 AM – 12:20 PM PST; Hall A-C (Moscone South)
Convener(s): Kelly Klima (Carnegie Mellon University) and Courtney St John (CRED, Columbia Earth Institute)

AGU 2013: Social Science Perspectives on Natural Hazards

//www.flickr.com/photos/tree_trunks/Learn about improving communication of and planning for natural hazards from a social science perspective at AGU2013.

The R/V Marcus G. Langseth: Ocean Explorer

American Geophysical Union Fall Meeting - Mon, 12/09/2013 - 11:41
R/V Marcus G. Langseth

Lamont-Doherty’s research vessel, the Marcus G. Langseth, in San Francisco bay.

The Marcus G. Langseth, a research vessel operated by Lamont-Doherty Earth Observatory, traverses the world’s oceans conducting marine seismic studies that contribute to new understanding of Earth systems. The ship typically spends half the year or more on research expeditions led by Lamont-Doherty scientists and colleagues from other research institutes.

Mentions of cruises may conjure up images of mammoth floating hotels and lounge chairs, but the cruises undertaken by earth scientists involve neither of those. Researchers who examine the seismic activity taking place beneath the sea can spend many weeks each year aboard ships deploying instruments and collecting data; these cruises often involve long days working in all manner of sea conditions.

At the American Geophysical Union (AGU) fall meeting, now taking place in San Francisco, scientists and students who use the Langseth for research expeditions, the ship’s operators and administers from Lamont-Doherty and the University-National Oceanographic Laboratory System (UNOLS), and National Science Foundation program managers, met on Dec. 8 for the Marcus Langseth Science Oversight Committee annual community meeting.

At AGU, the oversight committee’s goal was to review results of the ship’s recent expeditions and discuss future research cruises. This year, for the first time, the meeting included a young career scientists workshop, where graduate students and early career investigators who have worked aboard the Langseth gave short talks about their research. Lamont-Doherty presenters included graduate students Natalie Accardo, James Gibson and Shuoshuo Han; postdoctoral researcher Nathan Miller; associate research scientist Angela Slagle; and alum Danielle Sumy (Ph.D. ’11).

Paleoclimatologist Pratigya Polissar with sediment cores collected during his May 2012 Line Islands research cruise.

Paleoclimatologist Pratigya Polissar with sediment cores collected during his May 2012 Line Islands research cruise.

Their talks were followed by presentations by scientists on the Langseth’s recent and upcoming cruise activities. Highlights included a talk by paleoclimatologist Pratigya Polissar, who discussed his May 2012 cruise near the Line Islands in the central equatorial Pacific. Scientists on this cruise collected nearly 500 feet of sediment cores, which are being analyzed and used to gain new insight into the alternating El Niño and La Niña weather patterns that affect much of the globe. The oldest core recovered on Polissar’s expedition dates back more than 400,000 years, covering the last three glacial cycles.

Marine geophysicist Fernando Martinez (Ph.D. ’88) from the University of Hawai’i at Manoa reported on a cruise that he led to the Reykjanes Ridge in the North Atlantic Ocean in August 2013. The goal of the month-long cruise was to collect multibeam, magnetics and gravity data that will inform understanding of the evolution of the Reykjanes Ridge, a segment of the Mid-Atlantic Ridge just south of Iceland. This data will be used to test competing theories about what’s happening in this geologically fascinating area, with important implications for our understanding of geodynamic processes in the Earth.

Marine geophysicist Donna Shillington described a new research initiative that will use the Langseth to acquire large geophysical datasets in Atlantic waters as part of the Geodynamic Processes at Rifting and Subducting Margins (GeoPRISMS) project. The ultimate goal of GeoPRIMS is to investigate the coupled geodynamics, earth surface processes and climate interactions that build and modify continental margins over a wide range of timescales. The data Shillington and her group obtain during an upcoming cruise aboard the Langseth will be made available to the scientific community for various studies of the deep structure of the Eastern North Atlantic Margin. The project is also unique in that it features a large education and outreach component, which will train students and early career scientists to acquire and analyze seismic data.

The Langseth is scheduled to undergo maintenance in early 2014 before spending the remainder of the year on expeditions in the North Atlantic, including the GeoPRISMS cruise.

Visit the Marine Operations section of the Lamont-Doherty website to learn more about the R/V Langseth and the Observatory’s long history of seagoing exploration and discovery.

The R/V Marcus G. Langseth: Ocean Explorer

R/V Marcus G. LangsethThe Marcus G. Langseth, a research vessel operated by Lamont-Doherty Earth Observatory, traverses the world’s oceans conducting marine seismic studies that contribute to new understanding of Earth systems. The ship typically spends half the year or more on research expeditions led by Lamont-Doherty scientists and colleagues from other research institutes. Mentions of cruises may conjure up [...]

AGU 2013: Key Events From the Earth Institute

American Geophysical Union Fall Meeting - Fri, 12/06/2013 - 12:11

(Updated Dec. 10, 2013. James Hansen’s Frontiers of Geophysics talk has been RESCHEDULED to Wednesday, Dec. 11)

Scientists from Columbia University’s Earth Institute will present important research results and special events at the Dec. 9-13 San Francisco meeting of the American Geophysical Union, the world’s largest gathering of earth and space scientists. Here is a guide in rough chronological order. Unless otherwise stated, presenters are at our Lamont-Doherty Earth Observatory. Abstracts of talks and posters are on the AGU meeting program.  Reporters may contact scientists directly, or press officers: Kevin Krajick, kkrajick@ei.columbia.edu 917-361-7766 or Kim Martineau, kmartine@ldeo.columbia.edu 646-717-0134

# # # # #

The $5,000 ‘Dark Data’ Contest Award

Kerstin Lehnert, lehnert@ldeo.columbia.eduLeslie Hsu lhsu@ldeo.columbia.edu

As part of an initiative to save data in danger of dying within old floppy disks, tape drives or paper archives, judges will award a trophy and $5,000 to the team that has done the best job of finding and preserving such “dark data.” The International Data Rescue Competition is sponsored by Lamont-Doherty Earth Observatory’s Integrated Earth Data Applications project (which works to preserve dark data), and scientific publisher Elsevier. Sixteen teams from across the world have submitted entries. One group of seismologists has digitized Soviet magnetic recordings of Cold War nuclear tests in hopes of improving modern test-verification procedures. Another is a volunteer group that is digitizing handwritten weather observations from ship logs dating back hundreds of years.

Dark Data Talk: Monday, Dec. 9, 10:50-11:05 a.m., 2020 Moscone West. IN12A-03.

Award Ceremony: Monday, Dec. 9, 7-8:30 p.m., Twin Peaks Room, Intercontinental Hotel, 888 Howard St.

Read more about the contest

International Data Rescue Competition website and submissions

Integrated Earth Data Applications website 

 

 

The Dead Sea.

Drying of the Mediterranean and Mideast

Richard Seager seager@ldeo.columbia.edu

Nations surrounding the Mediterranean have been getting drier in the last decades, bringing record droughts to some places. Seager, a climate modeler, links drying in North Africa and Europe mainly to natural variability—but says there is evidence that drying of the Mideast is linked to overall climate warming. Further, based on changes in atmospheric circulation over the Mediterranean, he projects that the entire region from Spain through the Mideast may suffer increasing aridity in coming decades. This could happen not only during the usually dry summer, but during the crucial wintertime, when most rains now come in many places.

Monday, Dec. 9, 11:50 a.m.-12:05 p.m., 3003 Moscone West. GC12A-06 (Invited)

 

Climate Change: Spark of the Syrian Civil War?

Colin Kelley ckelley@ldeo.columbia.edu

From 2005-2010, Syria suffered its worst drought on record. Kelley and four colleagues say that natural weather variability played a role, but the root cause was probably a long-term shift in rainfall and heat caused by human greenhouse gas emissions. They say long-term atmospheric circulation changes increased the likelihood of drought in 2011 eight times over—and that increased warmth itself has directly caused drying of soils. While the causes of the war itself are complex, the drought brought food shortages, unemployment and disruption of rural social structures, driving some 1.5 million refugees from the countryside to the peripheries of cities, where discontent exploded into the ongoing bloodbath.

Monday, Dec. 9, 1:40-6 p.m., Posters A-C Moscone South. GC13A-1047

 

Global Farm Yields, Future Climate, and Conflict

James Rising jar2234@columbia.edu, Mark Cane mcane@ldeo.columbia.edu

More researchers are exploring the potential for swings in weather and climate to drive armed conflicts, often through crop failures that lead to violence. Looking at data from 1961-2008, Rising and Cane find that during times of high crop yields, conflicts have been less likely to break out. They plan to use this baseline information, along with data on crop varieties that grow in varying conditions, future climate scenarios, and economic and political conditions, to project future conflicts in different parts of the globe.  

Monday, Dec. 9, 1:40-6 p.m., Posters A-C Moscone South. GC13B-1069

(Related: Growing Susceptibility of the Global Food-Trade Network to Climate. Michael Puma, mjp38@columbia.edu. Monday, Dec. 9, 8 a.m.-12:20 p.m., Posters A-C Moscone South. GC11D-1038)

 

Scientists, Activism and the Impacts of Climate Change

 

James Hansen

James Hansen jeh1@columbia.edu

James Hansen, the outspoken former director of the NASA Goddard Institute for Space Studies, now leads a new policy-oriented climate-change program at the Earth Institute. Known for his efforts to turn science into action, he and colleagues recently made headlines with a study contending that the Intergovernmental Panel on Climate Change has vastly underestimated how quickly CO2 emissions must be slowed. Hansen will give three high-profile talks. On Tuesday, he presents the Union Frontiers of Geophysics lecture. On Thursday, he will speak on “Minimizing Irreversible Impacts of Human-Made Climate Change.” On Friday, his talk challenges the research community on “Communicating the Need to Avoid Dangerous Climate Change.” Among other things, he will discuss his past, present and planned efforts to get information to the public and to the highest levels of government.

RESCHEDULED TO: Wednesday, Dec. 11, 12:30-1:30 p.m., Hall E 134-135 Moscone North. U22C (Union Lecture)

Thursday, Dec. 12, 5:30-6 p.m., 104 Moscone South. GC44A-06 (Invited)

Friday, Dec. 13, 11:35 a.m.-12:05 p.m., 102 Moscone South. U52A-04

Earth Institute Program on Climate Science, Awareness and Solutions

 

CLimate Models Calendar clipClimate Models! The Pinup Calendar

Co-creators: Rebecca Fowler rfowler@ldeo.columbia.edu

Francesco Fiondella (International Research Institute for Climate and Society) francesco@iri.columbia.edu

Now you no longer have to dig through boring journal papers to learn all about your favorite climate scientists; just feast your eyes on the new 2014 Climate Models Calendar. Eye-popping portraits of 13 top Columbia University climate researchers in full regalia amid their natural habitat were conceived by bestselling photographer Jordan Matter (Dancers Among Us) and shot by fashion portraitist Charlie Naebeck. Calendar includes tasty inside info on the researcher of the month, such as favorite dataset or climate phenomenon. Individual dates are marked with famous climate/weather events, scientific meetings and other useful items. (There are 13 models because January 2015 comes as a bonus.) Models will be on hand to autograph calendars. (On sale through the Climate Models Calendar website, and at the Columbia M.A. in Climate and Society Program booth, no. 1329 in the Exhibit Hall.

Tuesday, Dec. 10, 1:40-6 p.m., Posters A-C Moscone South. ED23B-0725

Climate Models Calendar website

 

Did a 6th Century Comet Bring Global Famine?

Dallas Abbott, dallashabbott@gmail.com

Evidence from tree rings and ice cores suggest that parts of Europe, Asia and North America saw protracted cooling in the 530s, which has been linked to drought and famine. Some scientists hypothesize that Halley’s Comet may have caused this, by leaving a dust trail that the Earth later intercepted during its orbit. Dust in the air could have blocked the sun’s rays. Abbott finds evidence in ice cores drilled from Greenland: as much as 10 times more dust is found in the layer corresponding to 533 A.D. than at other intervals, she says. This dust is rich in markers of extraterrestrial origins such as nickel and iron oxide spherules. She finds that neither volcanism nor solar cycles can fully explain the cooling seen in various records during this decade. Furthermore, spikes of the ice-core dust appear to match the timing of the Eta Aquarid meteor shower, known to be triggered by Halley. 

Wednesday, Dec. 11, 8 a.m.-12:20 p.m., Posters A-C Moscone South. PP31B-1869

 

Burying CO2 in the Newark Basin:  Are There Earthquake Risks?

Natalia Zakharova nzakh@ldeo.columbia.edu

 In 2011, a consortium drilled a 1.5-mile deep hole off the New York State Thruway to study the rocks of the Newark Basin, which underlie parts of New York, New Jersey and Pennsylvania. Their goal: to understand the potential to store industrial carbon emissions, and the possible stresses on earthquake faults. Scientists are now analyzing data from this, and a second hole drilled this summer on the campus of nearby Lamont-Doherty Earth Observatory. Zakharova presents early results from the Thruway borehole; these suggest that shallow reservoirs contain critically stressed faults and are not good for injection; injecting fluids 1.2 kilometers or below may be safer.

Wednesday, Dec. 11, 1:40-6 p.m., Posters A-C Moscone South. S33D-2472

 

dsc_0040 BangladeshBangladesh: Shaking and Sinking

Michael Steckler steckler@ldeo.columbia.edu

For the past four years, a team from several universities has been studying the intertwined natural hazards of earthquakes, sea-level rise and sudden changes in river courses in Bangladesh, earth’s most densely populated nation. Now, detailed portraits of the forces driving these hazards are emerging. Principal investigator Michael Steckler gives an overview of how yearly loads of Himalayan sediment and water are interacting with rising sea level and a maze of underlying tectonic boundaries to create a system of dangers that could be set off by any number of triggers. Posters in a separate session paint a picture of hidden active faults around the capital of Dhaka, and how the delta on which Bangladesh sits is being twisted and squeezed by moving watery sediments and tectonic boundaries. 

Wednesday, Dec. 11, 1:40-1:55 p.m., 2005 Moscone West. EP33D-01 (Invited)

Related posters: Monday, Dec. 9, 1:40-6 p.m., Posters A-C Moscone South. T13D-2565 & T13D-2567

Short film on the project

 

Megadroughts: Signposts of the Past

Benjamin Cook bc9z@ldeo.columbia.edu

Edward Cook drdendro@ldeo.columbia.edu

Dendrochronologist Edward Cook has documented drought history in North America, monsoon Asia, and parts of Europe, North Africa and the Mideast. Tree rings going back many centuries before instrumental records reveal megadroughts covering vast regions and sometimes lasting more than 100 years—greater than anything seen in modern times. Such droughts were more common in the naturally warm period 600 to 1,000 years ago, he says. This suggests that greater warmth can push large climate systems into long-term aridity, raising the specter of megadroughts in the near future as climate warms. In a related talk, climate modeler Benjamin Cook (Edward’s son) delves into North America, starting with the devastating pan-continental drought of 2012. Similar to his father, he finds that droughts like this are rare, but not unprecedented, and occur most commonly during warmer times.  

Ben Cook: Monday, Dec. 9, 8 a.m.-12:20 p.m., Posters A-C, Moscone South. GC11A-0956

Ed Cook: Wednesday, Dec. 11, 4:45-5:05 p.m., 102 Moscone South. U34A-03

 

Turning CO2 to Stone

Juerg Matter jmatter@ldeo.columbia.edu

Some scientists say human-induced climate change could be mitigated by pumping industrial carbon dioxide underground; however, the fear of leaks is a major stumbling block. Matter’s group has been working on ways to turn pumped-down CO2 into a harmless limestone-like solid by harnessing natural chemical reactions underground. In the first field results from a pilot injection outside Reykjavik, Iceland, they have shown that the process can indeed work. The CarbFix project is dissolving CO2 in water and pumping it 500 to 800 meters down into a formation of basalt. Chemical monitoring shows that 85% of the CO2 reacts with the basalt within a year—a rate well beyond initial expectations. Scientists continue to monitor the storage reservoir.

Thursday, Dec. 12, 8 a.m.-12:20 p.m., Posters A-C Moscone South. V41A-2753

CarbFix website

AGU 2013: Key Events From the Earth Institute

dsc_0040 BangladeshScientists from Columbia University’s Earth Institute will present important research results and special events at the Dec. 9-13 San Francisco meeting of the American Geophysical Union, the world’s largest gathering of earth and space scientists. Here is a guide in rough chronological order.

IRI@AGU: Schedule of Events + Q&As

American Geophysical Union Fall Meeting - Fri, 12/06/2013 - 11:11

IRIatAGU

Four scientists and one PhD student from the International Research Institute for Climate and Society (IRI) are attending the 2013 American Geophysical Union’s Fall Meeting. Below are links to Q&As with each of the presenters and the schedule of their posters and presentations. For additional information about the scientists’ work, search the conference program for their names here.

The IRI is a research center at Columbia University’s Earth Institute dedicated to enhancing society’s capability to understand, anticipate and manage the impacts of climate in order to improve human welfare and the environment, especially in developing countries.

Pietro Ceccato Q&A

Poster: Development and Implementation of Flood Risk Mapping, Water Bodies Monitoring and Climate Information for Human Health (EP53A-0754)
Session: Earth and Planetary Surface Processes General Contributions Posters
Friday, Dec. 13
1:40 – 6 p.m.
Hall A-C (Moscone South)

Paula Gonzalez Q&A

Poster: Long-lead ENSO Predictability from CMIP5 Decadal Hindcasts (GC43D-1090)
Session: How Reliable and Accurate are CMIP5 Climate Simulations?
Thursday, Dec. 12
1:40 – 6 p.m.
Hall A-C (Moscone South)

Arthur Greene Q&A

Presentation: Climate scenarios for driving AgMIP models (GC31D-06)
Session: Improving the Understanding of climate Variability and Change in Agriculture: AgMIP, Tropical Farm Adaptation and Related Research
Wednesday, Dec. 11
9:15 – 9:30 a.m.
3001 Moscone West

Catherine Pomposi Q&A

Poster: Sahel rainfall variability as simulated by the CAM4 model and its associated atmospheric dynamics (A11G-0136)
Session: West African Monsoon and Its Modeling
Monday, Dec. 9
8 a.m. – 12:20 p.m.
Hall A-C (Moscone South)
_________________________

Presentation: Experiences in the New York Academy of Sciences STEM Mentoring Program (PA42A-08)
Session: Communicating the Relationship Between Policy Sciences, Natural Hazards, and Global Environmental Change
Thursday, Dec. 12
12:05 – 12:20 p.m.
2020 (Moscone West)

Andrew Robertson Q&A

Session (convener): Subseasonal to Seasonal Prediction: Bridging the Gap Between Weather and Climate
Monday, Dec. 9
8 – 10 a.m.
3010 (Moscone West)
_________________________

Poster: Diagnostics of Interannual-to-Interdecadal Climate and Streamflow Variability: Applications to Reservoir Management over NW India (GC11A-0960)
Session: Paleoclimate, Observations, and Models: Water Resource Management Under Climate Variability and Change
Monday, Dec. 9
8 a.m. – 12:20 p.m.
Hall A-C (Moscone South)
_________________________

Poster: Evaluation of Sub-monthly Forecast Skill from Global Ensemble Prediction Systems (A13E-0259)
Session: Subseasonal to Seasonal Prediction: Bridging the Gap Between Weather and Climate II Posters
Monday, Dec. 9
1:40 – 6 p.m.
Hall A-C (Moscone South)

IRI@AGU: Schedule of Events + Q&As

IRIatAGUFour scientists and one PhD student from the International Research Institute for Climate and Society are attending the 2013 American Geophysical Union's Fall Meeting. Below are links to Q&As with each of the presenters and the schedule of their posters and presentations.

Seismology as Performance Art

Jim Gaherty installs a seismic station in Masoko as a crowd looks on

Jim Gaherty installs a seismic station in Masoko as a crowd looks on

Ideally, seismic stations are sited in remote, quiet locations away from any possible cultural noise, especially people, who are very noisy (even if they are not New Yorkers). But other considerations besides peace and quiet are important for a good station, particularly security. As a result, we placed most of our stations in towns near schools, hospitals or town halls, where people could keep an eye on them.

We often attract crowds while installing our exotic seismic gear. Field work with an audience has pros and cons. It’s certainly somewhat distracting to labor and sweat under the sun, tinkering with wires and programming equipment with a big crowd in attendance. Some of the sites are in relatively tight spots, so the curious onlookers occupied much of our working space, making for very close quarters. Several days ago, we installed a station next to the village hall in Ndalisi as a small crowd looked on and an animated town meeting took place next door. Loud passionate speeches inside were matched by loud banging outside as we mounted a solar panel for our station on the roof.

P1040104

Students from the Ilindi elementary school watch from a distance

But there are very big upsides. People from the villages where we deployed stations have provided an enormous amount of help with building our sites. We have also had abundant opportunities to tell people what we hope to learn about the active tectonic environment where they live. Continental rifting here gives rise to geohazards such as earthquakes and volcanoes. Because we have tried to locate many of our sites near schools, we particularly hope to communicate our science to students and teachers. At the Matema Beach High School, students peppered us with questions as we installed our gear. Their school is just a stone’s throw from the Livingstone Mountains, the surface expression of a major rift fault that has caused large earthquakes. But our seismic installations admittedly may not be entirely positive; today at Kifule Secondary School, students took a long math exam inside while we were making a racket outside. But hopefully the pros out weigh the cons… Even at Kifule, students burst out of classroom after the test all smiles, so apparently we were not too disruptive.

Surface Views of the Southern East Africa Rift Inspire a Look Underground

P1040254

Kiejo volcano in the Rungwe Volcanic Province with a cinder cone

Driving around the Rungwe volcanic province in the southern East Africa Rift installing seismometers, we have the chance to observe first hand how geological processes in action create the most dramatic forms at Earth’s surface. Looming volcanoes flanked by cinder cones lie along the rift valley, often very close to rift faults. The Livingstone Mountains, the surface expression of a major fault system that bounds the rift to the east in this area, soar over 1.5 km over the valley below, including Lake Malawi (Nyasa).

P1040454

The Livingstone Mountains, which are the surface expression of a major rift fault

The remarkable geological structures evident above ground motivate us to look deeper in the earth. We see volcanoes in particular places at the surface, but where are magmas located at depth below the volcanoes and the rift? Likewise, we see dramatic faults that are helping to thin and break the crust at the surface, but how do they relate to stretching of the entire crust and lithosphere beneath this part of the East Africa rift? And how are the magmas and faults related to one another? These are the core scientific questions motivating our study of the rift around northern Lake Malawi (Nyasa). We hope to use data collected during this program, including the 15 seismic stations that we are deploying now around the Rungwe province, to answer these big questions.

Imaging beneath the southernmost volcanoes in the East Africa Rift

The last time we visited the southern part of the East Africa Rift, we were responding to an unusual series of earthquakes in December 2009 that shook northern Malawi. The faults responsible for these events had not produced any earthquakes historically, and thus caught everyone by surprise. The unexpected occurrence of earthquakes on these faults highlights our poor overall understanding of how the African continent is slowly stretching and breaking apart.

This time, we return to this part of the rift system as a part of a more comprehensive effort to understand the underpinnings of this continental rift using a spectrum of geological and geophysical tools and involving a big international team of scientists from the U.S., Tanzania and Malawi. In the coming three weeks, we plan to deploy ~15 seismometers in southwest Tanzania around the Rungwe volcanic province, the southernmost volcanism in the East Africa Rift system. These stations will record small local earthquakes associated with active shifting of faults and moving of magmas at depth. They will also record distant earthquakes that can be used to create images of structures beneath Earth’s surface and map the faults and magmas.

Rungwe seismic deployment

Map showing elevation and lake depth, locations of volcanoes (red triangles, from Smithsonian Global Volcanism Program), major faults (black lines) with planned locations for seismometers. We plan to deploy 15 stations (light blue circles) in the next three weeks around the Rungwe volcanic province. Dark blue circles show tentative locations of stations to be deployed in the summer of 2014.

 

The Langseth cruise is winding down!

Mapping the Galicia Rift off Spain - Thu, 08/01/2013 - 10:32

The Langseth Galicia 3D seismic cruise is winding down. By tomorrow we will be back at the dock in Vigo. Like most seagoing science, we will miss the ship experience, we will miss the new colleagues we have met, we will look forward to getting back on shore, and for many of us the awesome multi-year task of processing, interpreting, and publishing the boatload of data we have acquired.

This is an example of the data we have collected. Right is to the East and left is to the West. This is a cross section of the Earth about 65 km long. The blue is water. The water depth here is about 5 km. The red and gray colors are a cross section of the rocks below the water. The flat layers are sedimentary rocks. The lumpy bumps (that is a technical term!) consist of blocks of continental crust and of the mantle.

We thank the Langseth’s Captain and crew for making this possible! These are men and women who live on the sea, and who share their ocean world with us for a month or two. Every now and then, when you can walk 100 meters in a straight line, ask yourself, “Where is the Langseth now, and who is steering the ship, or keeping the engines running, or keeping the deck ship-shape, or providing good food, or every other important task on the ship?” Under your breath say thank you for the experience you had on Langseth.

We thank Robert and his technical team. They worked tirelessly to assemble the 24 km of hydrophone streamer that hears the reflections from the Earth, the 40 or so airguns that make the booms, and all the rigging it takes to tow them spread out behind the ship over 600 meters wide and 7000 meters long. That was just the start. Then they operated the electronic equipment that received the seismic data and recorded it for the scientists. Without them we could not do the science we love.

Thank you to the Science Party. We had a total of 20 scientists, including undergraduate students, graduate students, post-docs, researchers, and professors. On Leg 1 we had 14 scientists and on Leg 2 we had 10 scientists. Four scientists weathered both legs. Six joined us for Leg 2. I am very grateful for all your efforts on behalf of the Galicia 3D science. I hope that you learned a lot, had a good time, and met other scientists for the first time. I suspect that we will meet one another many times in the future.I look forward to that!


This is the Technical team and the Science team for Langseth Leg 2.
I want to thank the Protected Species Observers for sailing with us. They spent countless hours in the observing tower, high above any other part of the ship. They have sighted hundreds of whales, but most did not come close to the ship. It is windy and cold up there, but their role is important for making sure that collecting our scientific data does not interfere with the creatures who call the ocean home.

Thank you for sending your loved ones off on the Langseth. I can certify that they now know how to do their own laundry and to clean up their cabin before they leave the ship. During the weekly emergency drill, they run quickly up to the muster station on deck and put on safety gear. I recommend that you continue to enforce these behaviors ruthlessly! They will forget them if you let them slack-off. On the other hand, they did not have to cook their own food, or wash and dry their dishes. You will still have to work on these behaviors!

As I write this from the Langseth, we should remember that the Galicia 3D experiment goes on. Our colleagues from GEOMAR and University of Southampton will be on the FS Poseidon from 25 August to 10 September. They will be recovering the 78 Ocean Bottom Seismometers that are still on the bottom (on purpose!). They have been recording approximately 150,000 airgun array shots fired by the Langseth. I know what you are thinking. “How many total recordings of shots are recorded in all the OBS’s?” That would be about 11.7 million shot recordings. This will keep the OBS scientists busy for a while!

I particularly want to thank James Gibson for creating this blog. It has reached out to our friends and to strangers. We plan to keep the blog alive. This project will continue for years.


Best regards,
Dale Sawyer
Rice University

Behind the scenes of the ship

Mapping the Galicia Rift off Spain - Wed, 07/31/2013 - 13:26

This week we have been exploring all the parts of the ship we have not yet discovered and were lucky enough to get shown around the engine room and the bridge. It is evident that each area of a ship (bridge, engines, science etc.) has a group of people doing those specific jobs and that the combination of everyone doing their part keeps everything running smoothly; like cogs in a massive machine. 

The engine room control panel. With that many buttons no wonder it takes so much training to work in the engine room!
The engine room is located in the hull of the ship and is the biggest room on board by far, taking up about 2/3rds of the bottom deck. This is obviously a very important part of the ship because without it we would not be moving anywhere! The Langseth has 2 engines leading to 2 propellers and also 1 bow-thruster. There are so many different bits of machinery down there that it can take 4 years of studying to be qualified to work in the engine room. It is very loud and warm but surprisingly clean and tidy. There are also 2 compressors which are used to pressurise the air for the air guns that we tow. 

One of the very noisy compressors. It is hard to portray the size of these in a photo, they are huge!
The heat from the engines is used to produce all the hot water for the ship and the engine room also has machines for desalinising our water. Fuel usage is constantly monitored and fuel moved between all the many tanks spread around the ship to ensure even weight distribution. Even though we only travel at about 4 knots whilst acquiring data we burn between 5000-6000 Gallons of fuel a day due to the massive load of the equipment we are towing behind us.

One of the two engines
The bridge sits at the front of the ship on top of the main living quarters. From here it seems as if practically everything can be controlled. They drive the ship when we are not driving from the main science lab during acquisition, control the speed, can manage the safety aspects including all alarms and watertight doors and keep a look out for anything floating past that might get caught up in our seismic gear (so far buoys and pallets have been sighted). One very important job of the bridge is to communicate with other nearby vessels. Nobody would expect us to be towing 6km of streamers so we have to make sure we let other ships know with enough time to arrange safe passing, therefore avoiding collisions.

This is the main control panel in the bridge. There are screens for  navigation and
radar as well as all the speed controls. There are two smaller control panels
on the port and starboard sides of the bridge for work that
involves careful maneuvering e.g. picking up OBS's. 
The last seismic line is just being finished right now and then we can get ready to begin equipment recovery. It is about 40 hours until we are back on dry land again! 

Tessa Gregory
University of Southampton  

Binning is the name of the game

Mapping the Galicia Rift off Spain - Wed, 07/31/2013 - 04:44
As we come to the end of our cruise I thought that now would be a good time to talk about the way in which both seismic and multi-beam sonar data are quantified (basically nerd out). In both cases we "bin" the data into grid cells, which are predefined based on the resolution that we expect to achieve given the ideal data density of individual cells within the grid. 

A screen capture from the multi-beam sonar Seafloor Information System (SIS).
The image on the left shows swath coverage. The image on the right shows an active ping through the water column.
Multi-beam sonar (swath seafloor mapping) data are collected, gridded (binned) to the predefined cell size, and output in two flavors. Bathymetric grids, which are essentially 3D topographic maps, and Backscatter grids, which display the reflectivity of the seafloor. The reflectivity varies due to both incidence angle of the respective beams and the density of the surface (e.g. hard rock, sediment etc). As the ship moves along at a given velocity, the multi-beam sonar sends a "ping" from the transducers (transmitters) to the seafloor and then waits until the receipt of the last return to ping again. The ping rate (Hz or 1/seconds) is a function of the depth of the ocean as well as the sound speed through water (XBT's are useful!). The swath width also scales as a function of depth. Our average depth is ~4800m (2.98 miles), which allows for an achievable swath width of ~20km (12.43 miles!).

Swath coverage display of the backscatter (reflectivity of the seafloor) collected across a swath.
In order to gain insight on the density of the multi-channel seismic (MCS) data that we are collecting we use the Spectra software package. Spectra tracks the position of the ship, streamers, and air guns in real time using GPS and an acoustic network, and then bins the data accordingly within the predefined grid. The goal is to get an equal amount of seismic traces (reflected seismic waves) in each bin. The traces can then be stacked (combined), which increases the signal to noise ratio. Stacked traces within a bin are called "fold" and ideally represent traces from all offsets along the streamer in respect to the source.

A screen capture of the Spectra display. The image on the left shows active binning of the MCS data.
The image on the right shows the bins being infilled (filling holes).
We are getting to the end of the "No Mores," which means we are finished on Friday!! Stay tuned for a word from our Chief Scientist along with a look at the MCS data (and our cruise pic). 

James Gibson
Lamont-Doherty

Nom, Nom, Nom: Meals aboard the R/V Langseth

Mapping the Galicia Rift off Spain - Mon, 07/29/2013 - 08:15

After all these posts about how we live and work onboard the R/V Langseth you may just be wondering what sort of sustenance keeps us going during the long hours.  Well you’re in luck! The excellent cooks serve meals with a smile promptly three times a day at 7:20 am, 11:30 am, and 5:30 pm.  Breakfasts always include mountains of eggs, bacon, sausages, and pancakes and on special occasions scrumptious muffins.  Lunch usually comes with toasty grilled sandwiches, soup that warms your limbs, and crunchy French fries.  Dinner varies but commonly consists of a juicy steak or pork chop, rice, mashed potatoes that put even your Mom’s Thanksgiving potatoes to shame, and a delicious desert like cherry pie.  The salad bar is open 24 hours a day and even this far into the cruise still contains crisp spinach, olives, tomatoes, and a variety of other vegetables.
A sampling of the meals served onboard with cooked by the always smiling galley staff.
From left to right breakfast, lunch, and dinner.
In the center image the galley staff made up of June, Hervin, and Brian pose behind a lunch of pizza and soda.
We are now in the home stretch of our cruise, steaming furiously down our final sail lines to complete our 3D grid.  Can’t believe there’s only four more dinners until we set foot back on dry land!

Natalie Accardo
Lamont-Doherty

5 lessons I have learnt on my first scientific cruise

Mapping the Galicia Rift off Spain - Sat, 07/27/2013 - 09:40

I was sent to join this cruise half way through because a lot of the scientific party had to leave and nobody more qualified than me could be found at such short notice! I have never been on a cruise before and had no idea what to expect, or any idea how complex and time consuming 3D seismic acquisition is. I have learnt so much about the technical side of acquisition and a little bit about the processing side; however I have also gained a lot of non-scientific tips and tricks!

Here are my top 5 tips: 

1) ‘Boring science is good science’ – If you are bored on a 6 hour watch that is a good thing because it means that everything is running smoothly and good data is being collected. Having things to do is always a bad sign! Things have been running pretty well recently and as a result I have greatly improved my crossword skills.

2) Things will break, don’t panic! – This is a hand me down ship filled with second-hand instruments from industry vessels. Because of this a lot of the equipment is temperamental and repeatedly needs to be fixed. However, I have also seen instruments that have been offline for days randomly start working again so you never know!

3) Duck tape has a million uses – There is no end to the list of things duck tape is used for on this ship: keeping weights in place on streamers, keeping your laptop on the desk during bad weather, taping your ladder to your bunk so it doesn’t bang during rough weather and keeping ropes in place on the deck to name a few. It seems like any problem can be fixed with tape.
If you don't want your office chair rolling around or you need a cable tie just use tape!
4) Hoard food – When food you like is put out in the mess then take it while you can. A few days ago a gigantic tub of mini snickers and bounty bars was put out in the mess….I have never seen chocolate disappear so fast!

5) Taking a shower is the most dangerous activity on the ship – I recommend keeping either an elbow or hand on the wall at all times so you can feel when you start to move. I think taking a shower is probably the best form of exercise on the ship because of the amount of effort and energy it takes just to balance. Also, never soap the bottom of your feet in rough seas. That is probably classified as an extreme sport!

Tessa Gregory
University of Southampton

Free Time: Let's see what we have here!

Mapping the Galicia Rift off Spain - Fri, 07/26/2013 - 12:35
As Natalie told you, the Main Lab operates for 24 hours a day, but we have a 6 hour shift (nobody can work for 24 hours of course!).  So, what are we going to do in our free time? That is a great question!  Let me show you the Marcus Langseth's free-time facilities.

Located next to the Galley we have our Library which has a lot of good books (I was reading the Che Guevara's travel book before the beginning of this part II, I really want to finish it!) and these excellent chairs...they're really comfortable, believe me. You can also find a variety of mystery, fiction and scientific books on the shelves.
The library with a wide variety of books
Yeah, but John actually I'm not a book lover ...
No problem! This is what you need! A 42-inch TV screen and a big collection of movies and TV shows. Ah, and don't forget the PS3, which makes the crew's free-time fun.  I have to admit something to you, I've never used the movie room, but maybe sometime I will go there to catch a movie or documentary.
The movie room with seating for plentyBut if you're an athletic person, this is your place, the gym!
It's a little bit small, but if you think we're in the middle of the ocean, the luxury of having some equipment must be appreciated.
The gym ... be careful when the ship is moving!So, there is a treadmill, some free weights, etc. Be aware of the pitch, roll and heave! These are the movements made by the ship.  Instead of explaining them, I'll post an image which can perfectly illustrate what I'm trying to say.
The differences between pitching, rolling, and heavingFor those who appreciate an indoor sport, we also have a ping-pong table. It's located one level below the Galley, at the Main Deck. I didn't use this table either, but I'll launch a challenge: Try to play ping-pong during rough seas! Imagine how cool a ping-pong game is inside a ship facing waves of 5 or 7m (or even higher).
The ping pong table ... this could get interesting in rough seasThank you...or should I say Obrigado?

João (John) Pedro T. Zielinski
Complutense University of Madrid/Federal University of Santa Catarina

The beginning of the "No Mores"

Mapping the Galicia Rift off Spain - Fri, 07/26/2013 - 12:18
Today marks the final day before we start the infamous "No Mores".  No more Saturdays, then no more Sundays, and on and on until it is time for us to set a course towards dry land.  With almost two weeks behind us on this second half of the cruise we have only a handful of sail lines left to complete (see figure below).  Once we finish the lines we will head back down to the bottom half of our work site to fill in holes; isolated spots where we were unable to collect data due to strong currents or short-lived equipment problems.  After that it's back to port where we will wave farewell to the R/V Langseth as it steams towards the waters offshore of Iceland for another scientific adventure.
Don't forget to check out our progress as we fill in the sail lines here

Happy TGIF!

Natalie Accardo
Lamont-Doherty

Step into our Office: A tour of the main science lab in the R/V Langseth

Mapping the Galicia Rift off Spain - Tue, 07/23/2013 - 09:32
A panorama view of the main science lab
We left off last time with a tour of our sleeping quarters thus it seems only appropriate to now walk through the room where we spend most of waking hours; the main science lab.   Located one level below the gun deck, the main lab operates 24 hours a day controlling every aspect of data acquisition from monitoring the multichannel streamers and air-gun arrays to building the computers needed to process the terabytes of data that barrel in.  
An up close view of the numerous computer screens in the main lab
It can safely be said that when acquiring 3D seismic data during which approximately 6.5 terabytes of raw data will be recorded over 43 days you can never have enough computers.  In the main lab, laptops and computers occupy every surface.  Stand-alone computer monitors duck taped onto desks sit next to laptops anchored by bungee cables.  Power cords, Ethernet cables, and USB connections snake across tables in every direction periodically diving down into a dark power outlet. A bank of computer screens approximately 12 monitors wide and 3 monitors tall encircles nearly half of the lab.  These screens (39 in total) act as terminals that allow us to monitor and control a myriad of processes that are summarized in the image below.  Possibly of greatest importance are the terminals dedicated to “driving the ship.”   We aim to always have the four streamers following in perfect straight lines behind the ship however, cross-currents make this is a difficult charge.  Given the length of 6 km (3.7 miles!) and the weight of the streamers, it is akin to a toy boat towing four 23 m (75 ft) fishing lines straight behind it on a windy day. Thus to keep the streamers in the optimum orientation with respect to our acquisition line we continuously nudge the ship north and south while pulling the heads of the streamers with us. All of the steering is done from a combination of three monitors with the use of the software package “Spectra,” which in the simplest sense determines real time data coverage given the location of the air guns and the streamers. 
A labeled view of the bank of computer monitors that dominates the lab
Of equal importance are monitors that display the health of the four streamers and the two air-gun arrays.  We aim to keep the streamers at a constant depth relative to the air-gun arrays and also at a depth that keeps them protected from passing ship traffic.  In this part of the Atlantic fishing vessels are common and with our gear sitting kilometers behind our ship and 12 m (40 ft) beneath the sea surface one could see how a vessel might not know that it is there.  Therefore, whenever we see an approaching boat we implore them to keep a safe distance away both for the safety of their vessel and for our gear.  

The back of the lab where most of the preprocessing and quality control is done.
Additionally, we use this bank of terminals to monitor for the presence of critters in the water, the weather and sea conditions, and the health of the EM122 multi-beam.  Sitting back from the semi-circle of computers is another set of desks where the we, the students and scientists, stake our claim.  Outfitted with no-slip fabric and duck tape, we have covered the back of the room with our computers, which we use for pre-processing and quality control (QC) of the incoming data. 

That about covers the main lab, they keep it pretty cold down here for the sake of the computers so I’m headed up to grab another sweatshirt before I get frost bite.  Stay warm out there!

Natalie Accardo
Lamont-Doherty

What a difference a month makes!

Mapping the Galicia Rift off Spain - Sat, 07/20/2013 - 13:34

For those of you who have been following our adventure here's a comparison of the sea-state. I know that the few of us who have been out here for both halves definitely appreciate the difference, and for those joining for the second half it looks like smooth seas ahead!

Also, we have now reached 10,000 page views!! So thanks Mom (and everybody else).

James Gibson 
Lamont-Doherty

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