Geographic Area of Cruise: U.S. Southeastern Continental Margin, Blake Plateau
Date: June 13, 2019
Weather Data:
Latitude: 29°44.7’ N
Longitude: 080°06.7’ W
Wave Height: 2 feet
Wind Speed: 21 knots
Wind Direction: 251
Visibility: 10 nautical miles
Air Temperature: 26.6° C
Barometric Pressure: 1014.4
Sky: broken
As I sit here on the bow, with the wind blowing in my face, as we travel back to land, I think about the past two weeks. I think about all the wonderful people I have met, the friendships I have made, the lessons I have learned, and how I have grown as a person. The sea is a truly magical place and I will miss her dearly. Although I am excited to trade in some tonnage and saltwater for my paddleboard and Lake Erie, I will really miss Okeanos Explorer and everyone aboard.
My time aboard Okeanos Explorer has been wonderful. I learned so much about operating a ship, the animals we have seen, and about ocean exploration. I have stared into the eyes of dolphins as they surf our bow, watched lightening displays every night, seen Jupiter’s moons through binoculars, watched huge storm clouds roll in, seen how sound can produce visual images of the ocean floor, had epic singing and dancing parties as we loaded the XBT launcher, done a lot of yoga, learned a lot about memes, eaten amazing food, taken 3 minute or less showers, smacked my head countless times on the ceiling above my bed, watched the sunrise every night, done laundry several times because I didn’t bring enough socks, looked at the glittering plankton on the bow at night, and laughed a lot.
Words cannot express it all so below are some of my favorite images to show you how awesome this entire experience has been. I will not say goodbye to the sea and all of you but I will say, “Sea You Later. Until we meet again.”
Sunrise one morning.
Blowing out the candles on my birthday cake. Still so touched by the kind gesture. Photo Credit: Lieutenant Commander Kelly Fath, PHS
Meeting the ROV, Deep Discoverer. Pictured is Explorer in Training, Jahnelle Howe.
Looking at the dolphins on the bow.
Watching the dolphins surfing the bow waves. Photo Credit: Kitrea Takata-Glushkoff
The calm before the storm.
The final sunset with some of the amazing people I met at sea. Pictured from left to right: Jill Bartolotta (Teacher at Sea), Kitrea Takata-Glushkoff (Explorer in Training), and Jahnelle Howe (Explorer in Training). Photo Credit: Lieutenant Commander Faith Knighton
Geographic Area of Cruise: U.S. Southeastern Continental Margin, Blake Plateau
Date: June 10, 2019
Weather Data:
Latitude: 29°04.9’ N
Longitude: 079°53.2’ W
Wave Height: 1-2 feet
Wind Speed: 11 knots
Wind Direction: 241
Visibility: 10
Air Temperature: 26.7° C
Barometric Pressure: 1017.9
Sky: Clear
Science and Technology Log
As part of this mapping mission we are identifying places that may be of interest for an ROV (remotely operated vehicle) dive. So far a few locations have shown promise. The first is most likely an area with a dense mass of deep sea mound building coral and the other an area where the temperature dropped very quickly over a short period of time. But before I talk about these two areas of interest I would like to introduce you to some more equipment aboard.
CTD
CTD stands for conductivity, temperature, and depth. A CTD is sent down into the water column to collect information on depth, temperature, salinity, turbidity, and dissolved oxygen. Some CTDs have a sediment core on them so you can collect sediment sample. There is also a sonar on the bottom of the CTD on Okeanos Explorer that is used to detect how close the equipment is to the bottom of the ocean. You want to make sure you avoid hitting the bottom and damaging the equipment.
General Vessel Assistant Sidney Dunn assisting with CTD launch. Photo Credit: Charlie Wilkins SST Okeanos Explorer
Yesterday we used a CTD because the XBTs launched overnight showed a water temperature change of about 4°C over a few meters change in depth. This is a HUGE change! So it required further exploration and this is why we sent a CTD down in the same area. The CTD confirmed what the XBTs were showing and also provided interesting data on the dissolved oxygen available in this much colder water. It sounds like this area may be one of the ROV sites on the next leg of the mission.
Deep water canyon-like feature with cold water and high oxygen levels. Photo Credit: NOAA OER
ROV
ROV stands for remotely operated vehicle. Okeanos Explorer has a dual-body system meaning there are two pieces of equipment that rely on each other when they dive. The duo is called Deep Discoverer (D2) and Seirios. They are designed, built, and operated by NOAA Office of Ocean Exploration and Research (OER) and Global Foundation for Ocean Exploration (GFOE). Together they are able to dive to depths of 6,000 meters. D2 and Seirios are connected to the ship and controlled from the Mission Control room aboard the ship. Electricity from the ship is used to power the pair. A typical dive is 8-10 hours with 2 hours of prep time before and after the dive.
Seirios and D2 getting ready for a dive. Photo Credit: Art Howard, GFOE
Seirios lights up D2, takes pictures, provides an aerial view of D2, and contains a CTD. D2 weighs 9,000 pounds and is equipped with all types of sampling equipment, including:
Lights to illuminate the dark deep
High definition cameras that all allow for video or still frame photos
An arm with a claw to grab samples, such as rock or coral
Suction tube to bring soft specimens to the surface
Rock box to hold rock specimens
Specimen box to hold living specimens (many organisms do not handle the pressure changes well as they are brought to the surface so this box is sealed so the water temperature stays cold which helps the specimens adjust as they come to the surface)
D2 with some of her specimen collection parts labeled.
My favorite fact about D2 is how her operators keep her from imploding at deep depths where pressure is very strong and crushes items from the surface. Mineral oil is used to fill air spaces in the tubing and electric panel systems. By removing the air and replacing it with oil, you are reducing the amount of pressure these items feel. Thus, preventing them from getting crushed.
D2’s “brain” is shown behind the metal bars. The bars are there for extra protection. The panel boxes and tubes are filled with a yellow colored liquid. This liquid is the mineral oil that is used to reduce the pressure the boxes and tubes feel as D2 descends to the ocean floor.
D2 provides amazing imagery of what is happening below the surface. Like I said earlier, one of the areas of interest is mound-building coral. The mapping imagery below shows features that appear to be mound building coral and have shown to be true on previous dives in the area in 2018.
Multibeam bathymetry collected on this cruise that shows features which are similar to mound building coral that are known to be in the area. Photo Credit: NOAA OER
Mound-Building Coral
Mound-building coral (Lophelia pertusa) are a deep water coral occurring at depths of 200-1000 meters. They form large colonies and serve as habitat for many deep-water fish and other invertebrates. Unlike corals in tropical waters which are near the surface, Lophelia pertusa do not have the symbiotic relationship with algae. Therefore, they must actively feed to gain energy.
Large amounts of Lophelia pertusa, stony coral, found at the top of the crest of Richardson Ridge during Dive 07 of the Windows to the Deep 2018 expedition. Rubble of this species also appeared to form the mounds found in this region.
Personal Log
We saw whales today!!!! They went right past the ship on our port side and then went on their way. We weren’t able to see them too well, but based on their coloring, low profile in the water, and dorsal fin we think them to be pilot whales, most likely short-finned pilot whales. Pilot whales are highly social and intelligent whales.
Dorsal fin of a pilot whale
There was also the most amazing lightening show last night. The bolts were going vertically and horizontally through the sky. I think what I will miss most about being at sea is being able to see the storms far off in the distance.
Did You Know?
You can build your own ROV, maybe with your high school science or robotics club, and enter it in competitions.
High school ROV competition at The Ohio State University.
Geographic Area of Cruise: U.S. Southeastern Continental Margin, Blake Plateau
Date: June 8, 2019
Weather Data:
Latitude: 30°30.7’ N
Longitude: 078°11.2’ W
Wave Height: 3 feet
Wind Speed: 13 knots
Wind Direction: 150
Visibility: 10 nm
Air Temperature: 26.6° C
Barometric Pressure: 1015.9
Sky: overcast
Science and Technology Log
Throughout my blogs you have been hearing an awful lot about NOAA. But what is NOAA? NOAA stands for the National Oceanic and Atmospheric Administration. NOAA informs the public all about environmental happenings from the deepest depths of the ocean floor all the way to the sun.
NOAA was formed in 1970 as a federal agency within the Department of Commerce. It was the result of bringing three previous federal agencies together, U.S. Coast and Geodetic Survey, Weather Bureau, and U.S. Commission of Fish and Fisheries. Through research, NOAA understands and predicts changes in climate, weather, oceans, and coasts. Through outreach and education, NOAA shares the research with end users and the public with the purpose of conserving and managing coastal and marine ecosystems and resources (NOAA, 2019. https://www.noaa.gov/our-mission-and-vision).
In order to accomplish its mission, NOAA hires a whole slew of people including Commissioned Officers, administrators, career scientists, research technicians, vessel operators, educators, etc. These people may work on land or out at sea. In this blog I will focus on some of the NOAA careers at sea.
NOAA Commissioned Officer Corps (NOAA Corps)
The NOAA Corps is a descendant of the US Coast and Geodetic survey, the oldest federal scientific agency dedicated to surveying the ocean coast. Today, officers of the NOAA Corps command NOAA’s fleet of survey and research vessels and aircraft.
In order to be eligible to apply for NOAA Corps one must have a four-year degree in a study area related to the scientific or technical mission of NOAA. There are many other eligibility requirements and you can check them out here. Once you meet the requirements, you apply to the program, and if accepted you will head to the Coast Guard Academy in New London, Connecticut where you will attend a 19-week basic officer training class. Once officers graduate, they are assigned to sea duty for two years. After sea duty, officers rotate to land duty for three years. And the pattern continues as long as the officers choose to remain in the NOAA Corps.
NOAA officers fill many roles on Okeanos Explorer. Their primary role is to safely navigate the ship. All officers stand two 4-hour watches. During these watches, they are responsible for navigating and driving the ship, taking weather, and handling the ship per the requirements needed for the science mission whether it be for a series of ROV dives, mapping project, or emerging technology cruise. When not on watch, officers are responsible for collateral duties. There are many collateral duties, some of which are described below:
Safety officer: responsible for the safety drills and equipment.
Navigations officer: maintains charts, loads routes, plots routes on paper charts, updates electronic chart, and creates inbound and outbound routes for ports of call.
MWR (Morale, Welfare and Recreation) officer: responsible for fun activities when at sea or in port. These activities have included ice cream socials, movie nights, and baseball games.
Public affairs officer: Responsible for giving ship tours to the public, maintain the ships social media presence, and performs public outreach.
There are also many officer ranks (follow the ranks of the US Navy) aboard the ship. The entry level rank is ensign or junior officer and the highest rank is admiral, allowing for 10 ranks in total. In addition to rank classes, there are varying positions. Ensigns or junior officers are recent graduates of basic officer training and on their first sea assignments. They are learning how to navigate and drive the ship, the tasks associated with standing watch, and learning about the other collateral duties. The operations officer is responsible for all mission operations while at sea and in port. They serve as the liaison between the science team and the commanding officer. If project instructions change, the Operations Officer is responsible for managing operations, understanding requests or change and then speaking with the commanding officer to approve the change. They are also responsible for all logistics when in port such as shore power, vehicles, trash, potable water, fuel, and sewer. The next highest position (second in command) is the Executive Officer who also coordinates with many of the port duties, and is supervisor of the varying departments on the ship. They are also responsible for all paperwork and pay. The highest duty on the ship is that of Commanding Officer. They are ultimately responsible for mission execution and for the safety of the ship and people aboard.
The NOAA Commissioned Officers aboard Okeanos Explorer. From left to right: Ensign Brian Caldwell, Lieutenant Steven Solari, Lieutenant Rosemary Abbitt, Ensign Kevin Tarazona, Commander Eric Johnson, Ensign Nico Osborn, Lieutenant Commander Kelly Fath, Lieutenant Commander Faith Knighton, and Commander Nicole Manning.
Professional Mariners
Professional mariners provide technical assistance needed to support operations while at sea. They support the ship in five different expertise areas: deck, engineering, steward, survey, and electronics. More information about the professional mariners and job posting information can be found here. Some have attended maritime school to receive training or licensure to work aboard a ship at sea. Others get their training while at sea, take required training courses, and complete onboard assessments. These mariners that work their way up to leadership positions are known as hawse-pipers (for example, the Chief Boatswain, Jerrod Hozendorf, many years ago was a General Vessel Assistant and has worked up to the Department Head of the Deck Department.)
Deck
Deck hands and able bodied seamen who attend maritime school or training where they learn how to support ship operations, including but not limited to maintenance of the ship’s exterior, maintenance and operation of the ship’s cranes (places ROV (remotely operated vehicle) or CTD (conductivity temperature depth) in the water) and winches (lowers ROV and CTD into the water), and conducts 24/7 watches to ensure the safe operation and navigation of the ship. Augmenters also rotate through the fleet, while others are permanent crew on a ship.
The deck crew aboard Okeanos Explorer. Back row from left to right: General Vessel Assistant Sidney Dunn, Chief Bosun Jerrod Hozendorf, Able Bodied Seaman Angie Ullmann (augmenting), and General Vessel Assistant Deck Eli Pacheco. Front row from left to right: Able Bodied Seaman Peter Brill and Able Bodied Seaman Jay Michelsen (augmenting).
Engineering
The engineers aboard are responsible for the water treatment, air quality systems, and machines needed to make the ship move through the water. The also oversee the hydraulics of the cranes and winches. Engineers receive a four-year engineering degree at either a maritime academy or regular college. Depending on their degree, they will come aboard at different engineer expertise levels. Engineers move into higher level positions based on their days at sea and successful completion of licensing tests.
The engineers aboard Okeanos Explorer. From left to right: General Vessel Assistant Christian Lebron, Engine Utility Will Rougeux, Acting Chief Marine Engineer Ric Gabona, 3rd Assistant Engineer Alice Thompson (augmenting), Junior Utility Engineer Pedro Lebron, and Acting First Assistant Engineer Warren Taylor.
Stewards
The stewards on board are responsible for the preparation and management of the culinary services and the stateroom services such as bed linens. Tasks include meal planning, food purchasing and storage, food preparation, and oversight of the galley and mess.
The stewards aboard Okeanos Explorer. From left to right: General Vessel Assistant Eli Pacheco (assisting the stewards for this cruise), Chief Cook Ray Capati, and Chief Steward Mike Sapien.
Survey
Survey technicians are responsible for the operation of all survey equipment aboard the ship needed for mapping, CTD deployment, and ROV operations. Equipment includes echo sounders and meteorological and oceanographic sensors. They are also responsible for data quality control and processing, disseminating data to land data centers so it can be shared with the public, and working alongside the science team to assist with other data and equipment needs. A college degree is not required for survey technicians, but many of them have one in the fields of environmental or applied science.
Electronics
Electronic technicians are responsible for all electronics aboard such as the intercoms, radios, ship’s computers and internet access, sonars, telephones, electronic navigation and radar systems, and most importantly satellite TV! Chief Electronic Technicians rotate between land and sea, typically spending 2-3 months at sea.
Chief Electronic Technician Mike Peperato and Senior Survey Technician Charlie Wilkins pose with the CTD.
Personal Log
We saw dolphins today!!!! It was absolutely amazing. We believe them to be Atlantic Spotted Dolphins. Spotted you say? The one in the picture to the left is not spotted because it is less than one year old. They do not receive their spots until their first birthday. Spotted dolphins are very acrobatic. They enjoy jumping out of the water and surfing on the bow waves created by vessels. To date one of the best moments of the trip so far. Yay dolphins!!!!!
Atlantic spotted dolphins surfing the bow of the ship.
Did You Know?
Including all the NOAA officers and professional mariners aboard Okeanos Explorer, 12,000 people work for NOAA worldwide!
Geographic Area of Cruise: U.S. Southeastern Continental Margin, Blake Plateau
Date: June 5, 2019
Weather Data:
Latitude: 29°01.5’ N
Longitude: 079°16.0’ W
Wave Height: 2 feet
Wind Speed: 10 knots
Wind Direction: 128
Visibility: 10 nm
Air Temperature: 27.7°C
Barometric Pressure: 1021.3
Sky: few
Science and Technology Log
What is sonar?
Sonar is the use of sound to describe the marine environment. Sonar can be compared to satellites that use light to provide information about Earth, but instead of light, sound is used. It is used to develop nautical charts, detect hazards under the water, find shipwrecks, learn about characteristics of the water column such as biomass, and map the ocean floor. There are two types of sonar, active and passive. Active sonar is sonar that sends out its own sound wave. The sonar sends a sound wave (ping) out into the water and then waits for the sound to return. The return sound signal is called an echo. By assessing the time, angle, and strength of the return sound wave or echo one can learn many details about the marine environment. Passive sonar does not actively send out a sound ping, but rather listens for the sound from other objects or organisms in the water. These objects may be other vessels and these organisms may be whales or marine ecosystems such as coral reefs.
Sound waves move through the water at different speeds. These speeds are known as frequencies and the unit of measurement for sound is a hertz (Hz). Lower frequencies (example 18 kHz) are able to go farther down because they move slower and have more power behind them. It is like when a car goes down your street, pumping the bass (always seems to happen when I am trying to sleep) and you can hear it for a long time. That is because it is a low frequency and has longer wave lengths. Higher frequencies (example 200 kHz) move faster, but have less power. The sound waves should reach the bottom, an object, or biomass in the water column, but there may be no return or echo. High frequency sound waves are closer together. High frequencies give you a good image of what is happening near the surface of the water column and low frequencies give you a good idea of what is happening near, on, or under the ocean floor.
Type of Sonar on Okeanos Explorer
There are many types of sonar and other equipment aboard Okeanos Explorer for use during mapping operations. All have different capabilities and purposes. Together they provide a complete sound image of what is happening below us.
Kongsberg EM302 Multibeam Sonar
Multibeam sonar sends sound out into the water in a fan pattern below the hull (bottom) of the ship. It is able to map broad areas of the water column and seafloor from depths of 10 meters to 7,000 meters. Only the deepest trenches are out of its reach. It is the most appropriate sonar system to map seafloor features such as canyons and seamounts. The fan like beam it emits is 3-5.5x the water depth with a max swath range of 8 km. However, when you get to its depths below 5,000 meters the quality of the sound return is poor so scientists keep the swath range narrower to provide a higher quality of data return. The widest swath area scientists can use while maintaining quality is a depth of 3,300-5,000 meters. The user interface uses a color gradient to show you seafloor features (red=shallow and purple=deep).
Swath ranges for the multibeam sonar at various depths. The y-axis shows the water depth in meters and the x-axis shows the swath width in meters. Photo credit: SST Charlie Wilkins, NOAA Ship Okeanos Explorer
Some of the information that is collected using the multibeam sonar with labels describing their purpose. Photo Credit: NOAA OER
Backscatter
Backscatter uses the same pings from the multibeam. People use backscatter to model or predict physical or biological properties and composition of the sea floor. The coloring typically is in grayscale. A stronger echo looks brighter in the image. A weaker echo looks darker in the image. It gives you a birds-eye view of seafloor characteristics such as substrate density and seafloor features.
Top image is backscatter showing you a birds-eye view of the ocean floor. The bottom image shows you what it looks like when backscatter is overlaid over the bathymetry layer. You are able to see intensity of the sound return, but floor features are more noticeable. Photo credit: NOAA OER
XBT
An Expendable Bathy-Thermograph (XBT) provides you with information on the temperature gradients within the water. When the temperature profile is applied to a salinity profile (taken from World Ocean Atlas) you are able to determine sound velocity or the rate at which the sound waves can travel through the water. When sound moves through water it does not move in a straight line. Its path is affected by density which is determined by water type (freshwater or saltwater) and temperature. Freshwater is less dense than saltwater and cold water is denser than warm water. The XBT information accounts for sound refraction (bending) through various water densities. When near shore XBTs are launched more frequently because the freshwater inputs from land alter density of the water and temperatures in the water column are more varied. XBTs are launched less frequently when farther from shore since freshwater inputs are reduced or nonexistent and the water column temperature is more stable. However, ocean currents such as the Gulf Stream (affecting us on this cruise) can affect density as well. The Gulf Stream brings warm water from the Gulf of Mexico around the tip of Florida and along the eastern coast of the United States. Therefore, one must also take into account which ocean currents are present in the region when determining the launch schedule of XBTs.
Senior Survey Technician Charlie Wilkins and Explorer in Training, Jahnelle Howe, loading the XBT launcher. XBTs are launched off the stern of the ship.
Sound speed or velocity is determined by the density of the water, which is determined by temperature and salinity. Focus on the blue line in each graph. The first graph takes the information from the temperature and salinity graphs to determine sound speed. If we look at the first graph, we see that sound speed slows with depth. Sound speed slows because according to the second graph the temperature is colder making the water denser, thus affecting sound speed. Salinity does not vary much according to the third graph so its effect on density is most likely limited. Photo credit: NOAA OER
Simrad EK60 and EK80 Split-beam Sonar
Split-beam sonar sends out sound in single beam of sound (not a fan like the multibeam). Each transducer sends out its own frequency (example 18 kHz, 38 kHz, 70 KHz, 120 kHz, and 200 kHz). Some frequencies are run at the same time during mapping operations. Mapping operations typically do not use the 38 kHz frequency since it interferes with the multibeam sonar. Data collected with the use of the EK60 or EK80 provides information about the water column such as gaseous seeps, schools of fish, and other types of dense organism communities such as zooplankton. If you remember my “did you know” from the second blog, I discussed how sonar can be used to show the vertical diurnal migration of organisms. Well the EK60 or EK80 is the equipment that allows us to see these biological water column communities and their movements.
Water column information collected with the EK60 or EK80 split beam sonar. If you look at the first row you can see, in the image to the left, the blue dots are at the top and in the second image the blue dots are moving back down into the water column as the sun rises. The process of organisms’ movement in the water column at night to feed is known as vertical diurnal migration. Photo Credit: NOAA OER
Knudsen 3260 Sub-bottom Profiler
The purpose of using a sub-bottom profiler is to learn more about the layers (up to 80 meters) below the ocean floor. It works in conjunction with the sonar mapping the ocean floor to provide more information about the bottom substrate, such as sediment type and topography features. Sub-bottom data is used by geologists to better understand the top layers of the ocean floor. A very low frequency is used (3.5 kHz) because it needs to penetrate the ocean sediment. It will give you a cross section of the sea floor so floor features can be detected.
Cross section of the ocean seafloor shows you substrate characteristics. Photo Credit: NOAA OER
Telepresence
Telepresence aboard the ship allows the science team to get mapping products and raw data to land on a daily basis. The science team can also live feed data collection to shore in real time. By allowing a land based shore team to see the data in real time you are adding another system of checks and balances. It is one more set of eyes to make sure the data being collected looks correct and there are no issues. It also allows a more collaborative approach to mapping, since you are able to involve a worldwide audience in the mission. Public viewers can tune in as well. Support for the technology needed to allow telepresence capabilities comes in partnership with the Global Foundation of Ocean Exploration (GFOE). With GFOE’s help, the protocols, high-speed satellite networks, Internet services, web and social media interfaces, and many other tools are accessible when out to sea. The NOAA Office of Exploration and Research (OER) provides the experts needed to develop, maintain, and operate the telepresence systems while at sea, but also at shore through the Exploration Command Centers (ECCs) and the University of Rhode Island’s Inner Space Center.
Live interaction with Okeanos Explorer, Inner Space Center at URI/GSO, and a group of high school students. Photo credit: NOAA OER
All in all, the equipment aboard Okeanos Explorer is impressive in its abilities to provide the science team with a high quality and accurate depiction of the ocean floor and water column. The science team aboard is able to interpret the data, clean out unwanted data points, store massive data files on computers, and send it back to land daily, all while rocking away at sea. Very impressive and very cool!
Personal Log
I learned all about memes today. Apparently they are very popular on the ship. So popular, we are even in the middle of a meme contest. For those of you unfamiliar to memes like I was, a meme is a funny picture with a clever caption that makes you laugh or relates to something in your life. After my tutorial in meme making, we had a great time out on the bow of the ship playing corn hole and hanging out. The night was beautiful. The humidity subsided and there was a great breeze. After the sun set, I watched the stars come out and then went inside to learn more about the mapping process. I am starting to get a better understanding of what the science team is doing. You know the how and the why of it all. After I couldn’t keep my eyes open any longer, I made my nightly venture out onto the bow to look from some bioluminescence, the glittering of zooplankton in the night. A magical site. I will leave you wondering how the ocean glitters until one of my future blogs when I describe the process of bioluminescence.
General Vessel Assistant Sidney Dunn (left) and General Vessel Assistant Christian Lebron (right) playing corn hole on the bow at sunset.
Did You Know?
The SOFAR (Sound Fixing and Ranging) channel occurs in the world’s oceans between depths of 800 to 1000 meters in the water column. Because of the density and pressure around this channel, sound waves travel for an extended distance. It is thought that fin whales travel to this channel to communicate with other fin whales many kilometers away.
Geographic Area of Cruise: U.S. Southeastern Continental Margin, Blake Plateau
Date: June 3, 2019
Weather Data:
Latitude: 28°48.6’
Longitude: 079°26.8’
Wave Height: 1-2 feet
Wind Speed: 4 knots
Wind Direction: 158
Visibility: 10 nautical miles
Air Temperature: 27.9°C
Barometric Pressure: 1014
Sky: scattered
Explorer in Training
A part of this mission is to map previously unmapped area in the southeast Atlantic Ocean but another part is to train the next generation of ocean explorers. There are currently four Explorers in Training (EiTs) and one Knauss Fellow on the Okeanos Explorer who are learning about the process of mapping and processing data at sea.
The four EiTs aboard are Allisa Dalpe, Jahnelle Howe (EPP), Marcel Peliks, and Kitrea Takata-Glushkoff. All have come from ocean mapping or engineering programs at their universities and are very excited to be a part of this program.
EiTs heading to sea! From left to right: Katharine, Allisa, Marcel, Kitrea, and Jahnelle.
Allisa, originally from Cape Cod, Massachusetts is currently a Ph.D. candidate at the University of New Hampshire in Ocean Engineering. Her studies focus on the use of autonomous marine vehicles such as remotely operated vehicles (ROV). She is most interested in mission planning, decision making, and obstacle avoidance when mapping or collecting data. Allisa is a seasoned sailor as she participated in SEA Semester (Sea Education Association in Woods Hole) as a student and then returned as a deckhand when she sailed from Woods Hole to Cork, Ireland. Way cool! When I asked Allisa how this opportunity will compliment her Ph.D work she said that this mission will her develop algorithms for autonomous vehicles performing sea floor mapping. In layman terms, how to develop the blueprint for what decisions the robot will need to make while on a mission. Fun fact about Allisa, she plays the drums.
Jahnelle, originally from the Island of Montserrat in the Caribbean, is a Master’s student at City College in New York. Her focus of study is Earth and Atmospheric Science. She is interested in coastal resilience with specific focus on how coral bleaching events affect community structure through the use of remote sensing. Jahnelle became interested in her field of study because the country where she grew up had an active volcano. When the volcano erupted it would emit sulfur and carbon dioxide. She was interested in how it affected her community. Because of her childhood she is interested in how we affect the environment and how it affects us. Fun fact about Jahnelle, she is a creative writer of poems and short stories.
Marcel is currently in the process of completing his Master’s degree in Geological Oceanography at Moss Landing Marine Laboratories. A native to Poland, he moved to California in his teens and became interested in marine geology because he was fascinated with how much of the ocean is still unexplored. His thesis focuses on the use of multibeam sonar to map Monterey Canyon in California and asses how the canyon impacts sand transport on surrounding beaches. His dream career is to continue combining technology and geology to learn more about our planet. Fun fact about Marcel, he had his first corn dog at the age of 25.
Kitrea recently finished Bowdoin College with majors in Earth and oceanographic science and Russian. She will actually be finishing her credits in Russia come spring of 2020. Congratulations on almost being done! She is now interested in bringing her knowledge of geology and oceanography together by exploring the field of marine geology. When I ask Kitrea what this experience means for her she says that it is the opportunity to test run potential career paths within geoscience. More specifically to experience life at sea and delve deeper into the data collection and management side of mapping. So far she’s loving it all. Fun Fact about Kitrea, she is a ballet and modern dance teacher.
Knauss Fellowship
The Sea Grant Knauss Fellowship, named for John A. Knauss, one of Sea Grant’s founders and past NOAA Administrator, is a fellowship that places highly qualified graduate students in host agencies in the legislative or executive branches of the federal government. Interested students apply through their state Sea Grant program. Sea Grant is a nationwide program consisting of 34 programs in coastal areas (ocean and Great Lakes) focusing on research, outreach, and education. Sea Grant programs are federally supported by NOAA and a state university partner. For example, Ohio Sea Grant’s (my program) state university partner is The Ohio State University. Applicants who are selected for a Knauss Fellowship work for one year with their host organization. Many Knauss Fellows continue to work for their host organization or find similar positions with federal agencies after the fellowship. OER’s 2019 Knauss Fellow, Katharine Egan, who applied through Puerto Rico Sea Grant, is on board.
Katharine studied marine biology as an undergraduate student at the University of Rhode Island and received her Master’s degree from the University of the Virgin Islands in Marine and Environmental Science. A native to Pennsylvania, Katharine started studying marine science because the ocean was vastly different from where she grew up. She is a first generation college student and came from a landlocked area so marine science was tempting because of the adventures and new experiences it would bring. Since her time in school, Katharine has a multitude of experience studying coral reef ecology and geospatial analysis. In her Knauss Fellow role with OER, she is responsible for determining data gaps in OER’s standard operations and making OER data more accessible. Fun fact about Katharine, she read 54 books in 2018. Her favorite book out of the 54 was In the Distance by Herman Diaz.
To learn even more about the exploration team on board visit the OER website.
EiTs and the Knauss Fellow learning how to use the intercom system on the ship. The intercom is used for ship wide communication. From front to back: Kitrea, Katharine, Marcel, and Allisa.
Personal Log
Life at sea is pretty sweet. I am used to the movement of the ship. It is actually starting to put me to sleep so staying awake is challenging. My bed is super comfy and the room is actually pretty big. The food has also been amazing. We are very lucky to have such great cooks on board. There is also 24/7 access to ice cream. My hopes of shedding a few pounds have pretty much gone out the porthole.
My bed. I haven’t slept in a bunk bed since freshman year of college. I did my best job of making the bed, but it is pretty hard when you are holding on with one hand, swaying, and trying not to hit your head.
There are times when I forget we are on ship out at sea and then I look outside and remember where I am. It does get hard living in close quarters with so many people. I find that taking time to get outside to read or workout is super helpful. The weather so far has been wonderful. Sunny and warm most days with a nice breeze to keep it from getting too hot. My favorite time of the day is right before the sun sets when I do a yoga session to decompress from the day. After yoga I sit on the deck and watch the stars appear as I read my book. I have officially found my happy place.
My workout spot on the ship. A great view of the ocean makes the workout less challenging.
Did You Know?
Okeanos’ namesake is the Greek Titan god of the ocean. Well, actually, a river. The Ancient Greeks believed the ocean was a vast river circling the world.
