Posts Tagged ‘oceanography’

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South Pacific Bio-optics Cruise 2014: Tsunamis and the Open Ocean

April 2nd, 2014 by Aimee Neeley

As many of you probably heard, there was an 8.2-magnitude earthquake off the coast of Northern Chile on Tuesday night.  As with any earthquake around a coastal region or on the ocean floor, there is great concern about the formation of a tsunami.  A Tsunami is series of waves with a very large wavelength.  Think of a series of waves hitting a beach.  The distance between each wave hitting the shore is the wavelength.  Now picture a wavelength that is 100s of miles long!  Because the wavelengths are so long, the waves travel at very high speeds, around 600 miles per hour, in the deep ocean.  This is the speed at which a commercial jet plane travels!  However, the wave height (the height from the base of the wave at the water line to the top of the wave) is very small, maybe a few feet tall.  As you can imagine, a boat or ship in the open ocean wouldn’t even notice such a tiny wave.

Below is a screen shot from a CNN video report about the earthquake.  In this video you can see how the waves propagate out from the source of the earthquake out into the ocean (red arrow).

Wave propagation http://www.cnn.com/2014/04/01/world/americas/chile-earthquake/

Wave propagation
http://www.cnn.com/2014/04/01/world/americas/chile-earthquake/

The story changes, however, when the depth of the ocean decreases, such as when approaching land.  All of that energy in that fast wave gets slowed down and subsequently the height of the wave gets bigger, and sea level near shore can rise at least 50 feet!  Thankfully, our colleagues are out of harms way from tsunamis because they are in the middle of the deep, open ocean.

The ship and its inhabitants ARE, however, subject to waves that are created by storms and strong winds.  Joaquin made a video of the wave action that you can see below.  Here are  some freeze frame ‘action shots’ from the video.

https://www.youtube.com/watch?v=cBTORY0aalE&feature=youtu.be

Stage 1

Stage 1

Stage 2

Stage 2

Stage 3

Stage 3

Stage 4

Stage 4

And, lastly, I thought it would be good to show some pictures of how cold it is that far south and how challenging it can be to work outside on deck in the cold.  In this picture you can see icicles hanging off the ship during recovery of an IOP package deployment.

Water intrusion during recovery of the IOP package

Water intrusion during recovery of the IOP package

Mike and Scott are having a conversation as they wait for the IOP package to return to the surface of the ocean.  I wonder what they are talking about???

A very intense conversation ensues while waiting for the IOP package to return to the ocean surface

A very intense conversation ensues while waiting for the IOP package to return to the ocean surface

You can watch an entire IOP deployment below.

Lastly, when working so close to the continent of Antarctica, there must be a sighting of an iceberg.

Iceburg!

Iceberg!

 

 

Sources:

http://www.nws.noaa.gov/om/brochures/tsunami.htm

http://www.cnn.com/2014/04/01/world/americas/chile-earthquake/

South Pacific Bio-optics Cruise 2014: The First Station

March 30th, 2014 by Aimee Neeley

At approximately 60° South and 174° East the FSG members sampled their first official station of the field campaign.  The solid red line in the map below denotes the current ship track (as of March 27th).   The ship has not yet reached the P16S line that begins at 150° West (the blue circles on the map below).

p16s-cruisetrack copy

The FSG will deploy an IOP package at one station each day.  The FSG IOP package is an assemblage of instruments that collect data for temperature, salinity, depth, absorption of particles and dissolved components, and particle scattering.  The instruments are contained within a metal ‘cage’ that is lowered on a wire to a chosen depth in the water column.  The data collected by the instruments are saved to a type of hard drive located within the cage.  Before the cage can be deployed, weight must be added so that it can sink.

Adding weight to the IOP cage

Adding weight to the IOP cage

Here, the cage with all of the instruments is being lifted off the deck of the ship and lowered into the water.

Deploying the IOP package off the side of the ship

Deploying the IOP package off the side of the ship

And, sometimes, King Neptune decides to send a wave your way.  But that is why we wear our safety gear!

Scott catching a wave-It's all part of the job

Scott catching a wave-It’s all part of the job

The FSG also collects surface water samples in conjunction with the IOP package deployment.  A weighted tube is lowered over the side of the ship, and a large peristaltic pump gently transfers seawater to a large container (carboy).

Lowering tubing over the side of the ship to collect surface water

Lowering tubing over the side of the ship to collect surface water

Joaquin filling a carboy with surface water pumped off the side of the ship

Joaquin filling a carboy with surface water pumped off the side of the ship

The water is filtered and processed back in the laboratory on the ship.

Now, let’s take a moment to understand the significance and importance of hydrographic field campaigns.  Oceanic and atmospheric processes are tightly coupled.   Temperature and freshwater fluxes between the ocean and atmosphere are in control of climate variability.  A good example of this strong ocean-atmosphere relationship is El Nino Southern Oscillation or ENSO.  During an El Nino event, the temperature structure of the equatorial Pacific Ocean is disrupted.  The central equatorial Pacific Ocean becomes warmer than normal affecting tropical rainfall in Indonesia and global weather patterns. The objective of the Climate Variability and Predictability of the ocean-atmosphere system, or CLIVAR, program is to understand this dynamic coupling and model future ocean-atmosphere variability by collecting and analyzing ship-based global observations.  The International CLIVAR program is a continuation of its predecessors: the Tropical-Ocean Global Atmosphere (TOGA)  and the World Ocean Circulation Experiment (WOCE).  The TOGA program was formed in 1985 to study the relationship between the tropical ocean and the global atmosphere  with the ultimate goal of predicting variability on various time scales. The WOCE program began in 1990 with the objective to study global ocean circulation and its relationship to the global climate system over long time scales using global observations.  The US-CLIVAR program contributes to the international program as well as the World Climate Research Program.  You can learn more about the US-CLIVAR program here.

 

Image of global data from www.ewoce.org

Image of global data from www.ewoce.org

South Pacific Bio-optics Cruise 2014: The Field Campaign Has Begun!

March 24th, 2014 by Aimee Neeley

The guys are finally on their way!  The R/V Nathaniel B. Palmer set sail from Hobart, Tasmania on March 20, 2014 ( GMT +11 hours).  The science party is made up of a total 29 scientists, 9 of which are graduate students. The first Go-SHIP station is located at 67°S, 150°W. While in transit, scientists will deploy the first Bio-Argo float of the campaign, 6 days from sail.  An Argo float is a battery-operated, autonomous float that can move up and down the water column collecting temperature and salinity profiles up to a 2000m depth by pumping fluid into and out of a bladder to manipulate buoyancy.  A Bio-Argo can collect measurements of chlorophyll-a and backscattering, in addition to salinity and temperature profiles.  The deployment of Bio-Argo floats is particularly important for validating ocean color remote sensing data.  For more information about Argo floats, you can proceed to the following links:

How Argo Floats Work

Bio-Argo Floats

First sunset photo by Mike Novak

First sunset photo by Mike Novak

Setting up a scientific laboratory on a ship is no easy task.  Space is usually limited and you must be able to play well with others.  We have filtration equipment (the large wooden frames) set up to collect the biogeochemical parameters, i.e. phytoplankton pigments, particulate organic carbon and particle absorption.  The parameters are collected onto small paper filters and frozen for future analyses back at NASA Goddard.  We also have two instruments set up on board to measure colored dissolved organic matter (CDOM), which is like tea, compounds extracted from plant material that can flow out into the ocean via rivers.  While in transit to the first station Mike, Joaquin and Scott are busy collecting samples.

Mike Novak filtering samples

Mike Novak filtering samples

 

Particles on a filter pad

Particles on a filter pad

Joaquin Chaves preparing samples for storage

Joaquin Chaves preparing samples for storage

A major addition to this year’s field campaign is a ‘souped-up’ underway-sampling system built by none other than Scott Freeman, our optics expert on board the Palmer.  The set-up contains multiple instruments that collect dissolved and particulate absorption, CDOM fluorometry, chlorophyll and particle scattering at 660nm.   The system is connected to the ship’s seawater system that pumps clean seawater from <10m depth through the ship and then to faucets at which the water can be accessed.  The term ‘clean’ means the plumbing that facilitates seawater pumping to the laboratories is routinely checked for clogs and algae growth.

Scott Freeman and the underway sampling system

Scott Freeman and the underway sampling system

Lastly, a blog post isn’t complete without a gratuitous photo of macrofauna.  Here is a photo of a petrel taken by Joaquin Chaves.  Can anyone identify what kind of petrel this is?

Flying Petrel

Flying Petrel

South Pacific Bio-optics Cruise 2014: The South Pacific Bio-optics Cruise: An Introduction

March 20th, 2014 by Aimee Neeley

Three members of the Ocean Ecology Laboratory’s Field Support Group (FSG; Code 616) will embark on a 45-day journey from Hobart, Tasmania to Papeete, Tahiti on the icebreaker R/V Nathaniel B. Palmer (NBP).  The field campaign is part of the US Repeat Hydrography, P16S, 2014 under the auspices of GO-SHIP and sponsored by the US Climate Variability and Predictability Program (CLIVAR).  You can find more information about the program here.  The FSG will collect biogeochemical samples and bio-optical data across the South Pacific.  These data will eventually be ingested into NASA’s SeaWiFS Bio-optical Archive and Storage System (SeaBASS) and subsequently used for ocean color satellite validation activities.

During the next six weeks, I will be helping my colleagues chronicle their journey over the high seas.  They will share not only information about the science but also describe the daily life of a sea-going scientist.  I, too, participate in many of these campaigns and am very familiar with the NBP having sailed on it three times during my career.  Alas, I could not participate in the journey so must live vicariously through my colleagues.  Below, you will find the biographies of the three NASA scientists that are participating on this cruise: Joaquin Chaves, Scott Freeman, and Mike Novak. You can also follow the ship track here.

Joaquin Chaves, received his PhD in oceanography from the University of Rhode Island in 2004. For his graduate work he conducted research on estuarine biogeochemistry. He held postdoctoral positions at the Marine Biological Laboratory in Woods Hole, MA, and at Brown University, in RI, where he focused on the biogeochemistry of land use change in tropical forests, particularly in the Amazon region. He’s been a contract scientist at NASA-GSFC since 2009, where he has focused on ocean color satellite remote sensing and marine bio-optics. He has participated in ocean-going field campaigns to the Atlantic, Pacific, and Arctic Oceans, as well as the East China Sea.

Joaquin Chaves

Joaquin Chaves

A native Californian, Scott Freeman grew up in Salinas, near the Monterey Bay, and attended the University of California, San Diego. After a lengthy hiatus in New York City, he returned to college and received a B.S. in Biology from the City University of New York. He then attended the University of Rhode Island’s Graduate School of Oceanography, completed a master’s degree, and stayed in Rhode Island to work first for the URI, and then for Wetlabs, a manufacturer of oceanographic optical instruments. While in Rhode Island, he participated in many cruises and coastal exercises, including NASA’s Southern Ocean Gas Exchange Experiment (SO GASEX) and ONR’s Radiance in a Dynamic Ocean experiments (RADYO).

Since joining SSAI in 2011, Scott has participated in several field campaigns for NASA’s Ocean Ecology Laboratory, and is responsible for AOP and IOP data collection and processing. He lives in Alexandria, VA with his wife Heidi and sons Charles and Adrian. When not engaged in field research, one can find him playing bass for the Washington Metropolitan Philharmonic Orchestra.

Scott Freeman

Scott Freeman

Mike Novak grew up in Piscataway, New Jersey, about 30 miles southwest of Newark.  After graduating high school he attended the Richard Stockton College of New Jersey where he earned a B.S. degree in marine science.  After college, he attended graduate school at the University of New Hampshire where he earned an M.S. degree in Oceanography.  He worked as a researcher at UNH before relocating to the Washington D.C. area where he now works as an oceanographic researcher at NASA-GSFC.  When he is not sailing the high seas, he is also an avid musician playing at various venues around the D.C. area with his band Novakaine.

Mike Novak

Mike Novak

Salinity Processes in the Upper Ocean Regional Study (SPURS): SPURS Epilogue (The First)

October 15th, 2012 by Maria-Jose Viñas

By Eric Lindstrom

“Ships at a distance have every man’s wish on board.” — Zora Neale Hurston

Actual spurs.

So, we are back in port in the Azores Islands of Portugal. Knorr 209-1 was a fabulous voyage and it did feel that we had many a man’s wish on board. Those included wishes for our data collection from all the scientists involved in SPURS and well wishes from all the family members of the expedition and finally the good wishes of you, my blog audience.

The Knorr SPURS science group.

Thank you all for following my SPURS adventure so far. The saga continues for another year. We have instruments in the water and more expeditions ahead (in March and September 2013). Each expedition will be slightly different in nature but overall working toward the SPURS goal of understanding the surface salinity maximum in the Atlantic and the water cycle on the planet. I’ll be going into a different mode of blogging now, to provide you updates on the science and the observations as the year goes along. With good fortune, I will get back to sea for the final leg of SPURS in September 2013. If you would like another voyage blog from the Sargasso Sea in 2013, let your voices be heard in the comments section below!

After several days of riding a lumpy swell from Tropical Storm Oscar, we were greeted by the magnificent sight of greenery and civilization at Ponta Delgada on the island of São Miguel.

Ponta Delgada’s water front.

Panorama of Ponta Delgada’s waterfront.

The Knorr in Ponta Delgada.

The expedition was a success scientifically.  We got our sensor web in the water for the coming year: three moorings, 25 Argo floats, 18 surface drifters, three Wavegliders, three Seagliders, and a Lagrangian Mixed Layer Float. We completed a wide variety of shipboard deployments: 764 Underway CTD casts, 100 CTD/LADCP Stations, 30 Vertical Microstructure Profiles, 33 AUV missions, three Slocum glider turbulence missions, and a full suite of continuous measurements including ocean velocity profiles, thermosalinograph and meteorology/fluxes. We accomplished the objectives we had laid out for us – deploy the sensor web (week 1), do a control volume survey around the moorings (week 2), and map a mesoscale ocean feature (week 3). We were able to squeeze in some extras, like a 24-hour time series in the saltiest water and pick up a glider from the French expedition in August.

The expedition was a success for NASA and WHOI.  We even caught the attention of the International Space Station and had a great 30-minute chat with Commander Sunita Williams about research in sea and space and the strong connections between the space program and oceanography.

The expedition was a success in interagency cooperation. SPURS is led by NASA, but has enormously important contributions from NSF, NOAA, and the Office of Naval Research.  It takes a village to put on a good oceanographic process study!

I created a “SPURS Illustrated Campaign Summary” from our Knorr expedition. I will make it available to all of you as part of a future post. There will also be movies available from the Space Station call and from the expedition, which are still in the editing process.

Your questions and comments on SPURS are always welcome. Use the comments section of any of the posts and I will get the message. Your interest and curiosity provides directions for future blogs and helps me put into words some of the technical aspects of SPURS that may not be fully understood.

Thanks you all for again following along on our Knorr SPURS expedition. There is much more to come, so stay tuned!

Notes from the Field