atmosphere – NOAA Teacher at Sea Blog

June 14, 2023July 9, 2023

Laura Guertin: Stitch the Sky at Sea, June 14, 2023

NOAA Teacher at Sea

Laura Guertin

Aboard NOAA Ship Oscar Dyson

June 10 – June 22, 2023

Mission: 2023 Summer Acoustic-Trawl Survey of Walleye Pollock in the Gulf of Alaska

Geographic Area of Cruise: Islands of Four Mountains area, Western Gulf of Alaska
Location (2PM (Alaska Time), June 13): 54^o 19.3929′ N, 161^o 35.5129′ W

Data from 2PM (Alaska Time), June 13, 2023
Air Temperature: 7.2 ^oC
Water Temperature (mid-hull): 6.5^oC
Wind Speed: 9.25 knots
Wind Direction: 144.73 degrees
Course Over Ground (COG): 254.48 degrees
Speed Over Ground (SOG): 11.34 knots

Date: June 14, 2023

As a trained scientist and educator who is passionate about communicating science, I’m always thinking of different ways we can tell stories and share our data with non-scientists and students. I have been crocheting temperature data since 2017 and sharing my temperature scarves that record daily maximum temperature values for a location. In 2018, I began a journey of quilting science stories (see my blog post on the Teacher At Sea Alumni Association (TASAA) blog, Sharing Stories of the Louisiana Coast Through Quilts). While I’m on Oscar Dyson, I’m going to be creating another type of story/data visualization, based upon the observations I make looking up at the sky – and I hope you will join me!

A full description of my Stitch the Sky At Sea project is available on the TASAA blog. But note that you can do any variation, use any colors, select any style of stitching… the project is yours to create! I started the project with my visual observations back home (Philadelphia, PA) on June 1, before I flew to Alaska. This is the color scale I’m using and selecting which yarn matches what I’m seeing in the sky. It has been overcast my entire time in Kodiak (AK) so far – you can see the jump in color!

A close-up view of a left hand holding a crochet hook and several rows of stitches in gray yarn. This image has text overlain that reads: Stitch the Sky At Sea Project

A collage of three images: the top two are images of blue skies at locations in Pennsylvania (labeled PA) and Washington (labeled WA). The bottom image shows a row of stitches and bold blue yarn.

Photos: Announcing the Stitch The Sky At Sea Project (top left); Photos of blue skies at my home (Philadelphia) and where I had a one-night layover during travel (Seattle) with rows stitched onto the beginning edge (top middle); Photo of what the sky has looked like every day I was in Kodiak before sailing – completely clouded over (top right); The five colors of yarn I’m using for the five shades of the sky I’m observing the same time each day (bottom center). The yarn is from The Tempestry Project and in the colors of Aurora (top left), Downpour (top right), Cumulus (middle), Nimbus (lower left), Nebula (lower right).

This table will include my recorded observations. Again, you can stitch what I’m seeing, stitch what you are seeing in your location on the same date – or stitch both data for comparison! I’ll continue stitching through the end of the month to see what I can learn from my observations between these locations.

June	Location	Sky color observed (by myself)	NOAA’s sky cover value	Notes
1	PHL	bright blue	0.1	At home, waiting to depart
2	PHL	bright blue	0.2
3	SEA	bright blue	0.1	Flew out of Philly early AM, day in Seattle
4	Kodiak	dark gray	1.0	Arrived in Kodiak, stay in hotel
5	Kodiak	dark gray	1.0
6	Kodiak	dark gray	1.0
7	Kodiak	dark gray	1.0
8	Kodiak	dark gray	1.0
9	Kodiak	dark gray	1.0
10	transit	white	0.9	Departed Kodiak, day of transit
11	transit/ shelter	light gray	0.9	transit/sheltering in Larsen Bay
12	transit	white	0.3	restart transit at 5AM
13	transit	light gray	0.9	*starting this date, sky cover value as reported in Cold Bay
14	transit	dark gray	1.0	Arrival at first transect site, survey begins
15	transects	dark gray	0.9
16	transects	light blue	1.0
17	transects	bright blue	0.4
18	transects	light gray	0.7
19	transects	dark gray	0.9
20	transects	dark gray	0.8
21	transit	dark gray	1.0	*sky cover value as reported in Kodiak
22	dock in Kodiak!	dark gray	1.0	Left Kodia at 4PM (AK Time), flew to Anchorage, then Seattle
23	SEA	light blue	0.3	Travel day, Seattle to Philadelphia – sky cover for Seattle
24	PHL	dark gray	0.9	*sky cover for Philadelphia
25	PHL	white	0.6
26	PHL	light gray	0.9
27	PHL	white	0.9
28	PHL	light blue	0.6
29	PHL	light gray	0.6	[Canadian wildfire smoke covering the region today 🙁 ]
30	PHL	light gray	0.6

I will be taking photos of the sky and plotting them along with the ship location in this Google Earth file (just the days we are at sea – not the days on land).

I’m excited to be able to wear so many hats while at sea – scientist, educator, communicator, and crafter! If you decide to stitch along, please share your work!

Short crocheted piece in a rectangular shape in colors of blue, white, and dark blue/gray — Completed stitching, as of June 13. The top two rows are in a non-project color to mark the beginning. Each row is a double-crochet in the color I’m observing as I look to the sky each day at approximately the same time (~10:30AM Alaska Time).

June 28, 2016March 12, 2021

Julia Harvey: More to a Mooring than meets the Eye, June 26, 2016

NOAA Teacher at Sea

Julia Harvey

Aboard NOAA Ship Hi’ialakai

June 25 – July 3, 2016

Mission: WHOI Hawaii Ocean Timeseries Station (WHOTS)

Geographical Area of Cruise: Pacific Ocean, north of Hawaii

Date: June 26^th, 2016

Weather Data from the Bridge

Wind Speed: 15 knots

Wind Direction: 100 degrees (slightly east southeast)

Temperature: 24.5 degrees C

Barometric Pressure: 1014.7 mb

Science and Technology Log

One of the primary objectives of this WHOTS project is to deploy WHOTS-13 mooring. This will be accomplished on our second day at sea.

Site of Mooring-13 courtesy of WHOTS Project Instructions — Site of Mooring-13
(courtesy of WHOTS Project Instructions)

The mooring site was chosen because it is far enough away from Hawaii so that it is not influenced by the landmasses. Mooring 13 will be located near mooring 12 in the North Pacific Ocean where the Northeast Trade Winds blow. Data collected from the moorings will be used to better understand the interactions between the atmosphere and the ocean. Instruments on the buoy record atmospheric conditions and instruments attached to the mooring line record oceanic conditions.

A look at interactions between the atmosphere and the ocean. [R. Weller, WHOI]

There is a lot more going on than just plopping a mooring in the sea. Chief Scientist Al Plueddemann from Woods Hole Oceanographic Institution and his team began in-port prep work on June 16^th. This included loading, positioning and securing the scientific equipment on the ship. A meteorological system needed to be installed on the Hi’ialakai to collect data critical to the mission. And then there was the assembly of the buoy which had been shipped to Hawaii in pieces. Once assembled, the sensors on the buoy were tested.

Meteorological Station on the Bow — Meteorological Station

As we left Oahu, we stopped to perform a CTD (conductivity/temperature/depth) cast. This allowed for the testing of the equipment and once water samples were collected, the calibration of the conductivity sensors occurred.

Sunday, June 26^th, was the day of deployment. Beginning very early in the morning, equipment was arranged on deck to make deployment efficient as possible. And the science team mentally prepared for the day’s task.

Predeployment — The deck before deployment began. The buoy is the blue item on the left.

Promptly at 7:30 am, deployment began. The first stage was to deploy the top 47 meters of the mooring with sensing instruments called microcats attached at 5 meter intervals. A microcats has a memory card and will collect temperature, conductivity and pressure data about every three minutes until the mooring is removed next year.

Sensing instruments for the morring — Microcats for recording oceanic conditions

readied microcats — Microcats readied for deployment. They are lined up on the deck based on their deployment depth.

This portion of the mooring is then attached to the surface buoy, which is lifted by a crane and lowered overboard. More of the mooring with instruments is lowered over the stern.

The remainder of the mooring is composed of wire, nylon, 68 glass balls and an anchor. At one point, the mooring wire became damaged. To solve this problem, marine technicians and crew removed the damaged portions and replaced the section with wire from a new spool. This process delayed the completion of mooring deployment but it showed how problems can be solved even when far out at sea.

After dinner, the nylon section of the rope was deployed. Amazingly, this section is more than 2000 meters long and will be hand deployed followed by a section of 1500 m colmega line. It was dark by the time this portion was in the water. 68 glass floats were then attached and moved into the water. These floats will help in the recovery of the mooring next year. The attachment to the anchor was readied.

glass floats for recovery — These glass floats will help when the mooring is recovered next year.

The anchor weighs 9300 pounds on deck and will sit at a depth of 4756 meters. That is nearly 3 miles below the ocean surface. The crane is used to lift the anchor overboard. The anchor will drop at 1.6 m/s and may take about 50 minutes to reach the bottom. As the anchor sinks, the wire, nylon and the rest of the mooring will be pulled down. Once it reaches the bottom, the mooring will be roughly vertical from the buoy to the anchor.

Personal Log

I sailed aboard NOAA ship Oscar Dyson in 2013 so I already had a general idea of what life aboard a ship would be. Both ships have workout areas, laundry facilities, lounges, and of course messes where we all eat. But on the Hi’ialakai, I am less likely to get lost because of the layout. A door that goes up is near a door that goes down.

On our first day aboard, we held two safety drills. The first was the abandon ship drill. As soon as we heard 6 short and 1 long whistles, we grabbed our life jacket, survival suit and a hat. We reported to our muster stations. I am assigned to lifeboat #1 and I report the starboard side of 0-3 deck ( 2 levels up from my room). Once I arrived, a NOAA officer began taking role and told us to don the survival suit. This being my first time putting the suit on, I was excited. But that didn’t last long. Getting the legs on after taking off shoes was easy as was putting one arm in. After that, it was challenging. It was about 84 F outside. The suit is made of neoprene. And my hands were the shapes of mittens so imagine trying to zip it up. I finally was successful and suffered a bit to get a few photos. This was followed by a lesson for how to release the lifeboats. There are enough lifeboats on each side of the ship, to hold 150% of the capacity on board.

Survival Suit & Julia — Abandon Ship drill with Survival Suit

Safety is an important aspect of living aboard a NOAA ship. It is critical to practice drills just like we do at school. So when something does happen, everyone knows what to do. A long whistle signals a fire. All of the scientists report to the Dry Lab for a head count and to wait for further instruction.

I am reminded of how small our world really is. At dinner Saturday, I discovered one of the new NOAA officers was from Cottage Grove, Oregon. Cottage Grove is just a short drive south of Eugene. She had a friend of mine as her calculus teacher. Then a research associate asked me if I knew a kid, who had graduated from South Eugene High School and swam in Virginia. I did. He had not only been in my class but also swam with my oldest son on a number of relay teams growing up. Small world indeed.

Did You Know?

The Hi’ialakai was once a Navy surveillance ship (USNS Vindicator) during the Cold War. NOAA acquired it in 2001 and converted it to support oceanic research.

December 19, 2004March 18, 2021

Mary Cook, December 19, 2004

NOAA Teacher at Sea
Mary Cook
Onboard NOAA Ship Ronald H. Brown
December 5, 2004 – January 7, 2005

Mission: Climate Prediction for the Americas
Geographical Area: Chilean Coast
Date: December 19, 2004

Location: Latitude 25°07.83’S, Longitude 81°54.62’W
Time: 0830

Weather Data from the Bridge
Air Temperature (Celsius) 19.04
Water Temperature (Celsius) 19.42
Relative Humidity (percent) 56.95
Air Pressure (millibars) 1018.17
Wind Direction (degrees) 155.6
Wind Speed (knots) 15.91
Wind Speed (meters/sec) 7.99
Sunrise 0734
Sunset 2116 (9:16 pm)

Questions of the Day

Why is the sunset so late in the day?

Positive Quote for the Day

“The world of achievement has always belonged to the optimist.” J. Harold Wilkins

Science and Technology Log

We tossed the last of fifteen drifting buoys this morning! It’s not the end, but the beginning of a wonderful new program. I’d say the Adopt-a-Drifter program got underway with a big splash! Teachers and their students around the world can adopt a drifting buoy just like my students at Southside Middle School in Batesville, Arkansas. They can map its path as it goes with the flow of the ocean currents. These drifting buoys also provide sea surface temperature and air pressure. This information can be utilized to gain a better understanding of the global oceans. I watched as Jeff and Bob deployed another Argo float. These floats are lowered over the back of the ship and when the quick-release mechanism comes in contact with the water, the powder in a small device dissolves and this releases a spring that unhinges the float from the straps. The straps are pulled back onboard as the ship leaves the Argo float in its wake.

I sat down and had a conversation with Chief Scientist Dr. Robert Weller of Woods Hole Oceanographic Institution about the importance of oceanic/atmospheric studies. He made some very good points that highlighted the fact that when just 1ºC of heat energy is released from the ocean water into the atmosphere it affects the air flows for thousands of miles. This then can be like a domino effect and continue around the globe influencing weather patterns for people everywhere.

At 2:00 we interviewed Richard Whitehead, Chief Steward. Richard is over the food preparation in the galley. Richard shared that he has been working on ships for over 40 years and has had several trainings for the position he now holds. He said that the menus were developed based on nutritional guidelines and availability of produce. Richard shared with us that they keep the produce fresh for weeks by keeping it very cool and placing it in special bags that slows the deterioration. He also said that there are many safety issues that concern food preparation on a moving ship. All the pots and pans are deep, there are railings on the stovetop, and special care must be taken with knives. The countertops must be covered with anti-slip cloths to keep everything from sliding around. He also said that they consider the weather when deciding what to prepare because you wouldn’t want to bake a cake while the ship was moving through rough waters.

We changed “6:00 Science on the Fantail” to “6:00 Science in the Van on the Bow” because we wanted to interview Jason Tomlinson of Texas A & M about his work with aerosols. First of all, Jason explained that an aerosol is not a spray can. It is a small particle in the air. Jason showed us the Tandem Differential Mobility Analyzer (TDMA). It looks like a mad scientist’s invention with wires, tubes, canisters, and radioactive components! It is one of the best devices in the world for analyzing small particles in the air. It draws in air from outside then dries the air. It then separates the particles according to size. Jason said that these particles are too small to see with the naked eye but they have a great influence on cloud formation and cloud life length. The TDMA can determine what the particles are made of by adding moisture or by adding heat. The TDMA costs about $70,000! He also showed us the Aerodynamic Particle Sizer (APS) which analyzes larger particles. They mostly get sea salt and dust out here in the ocean. Jason said that there’s a mystery about the sea salt and its influence on clouds. The APS costs about $35,000. He also said that occasionally they take in the ship’s exhaust and that destroys their data for that particular time. He concluded by saying that it all gets back to climate change and using these data to make better models for predictions.

After our interview with Jason, we ran outside to glimpse San Felix and San Ambrosio Islands! Our first land sighting in over two weeks! These small islands, located about 300 nautical miles from Chile, are volcanic in origin. They are basically huge, desolate rocks protruding up from the ocean floor. As far as I could tell nothing is growing on them. Seafaring birds do nest on the cliffs. Since 1975 the Chilean Navy has had an installation on San Felix Island where they operate a short airstrip, a weather station and a tide station.

Personal Log

I’m just beginning to realize that this trip is nearly over. We only have four days left. I knew it wouldn’t go on forever but as the old saying goes “time flies when you’re having fun”. What a superb voyage this has been for me-a voyage that is continuing my personal quest to search out the majesty of Earth. In doing so it is my heart’s desire to absorb the inexplicable magnificence of our Earth. I want to be permeated with awe for the splendor as I soak it in with my eyes and ears and nose and skin. I am amazed. How can I take it all in? Where was I when the Earth was formed and hung in the nothingness of space? From where did this splendor come? Clouds and rain and snow and hail are amazing! Mountains and valleys and canyons and caves are amazing! Oceans and rivers and glaciers and springs are amazing! Rocks and minerals and soil and sand are amazing! People and animals and languages and ideas are amazing! And they all work together in a symphony of overwhelming magnitude. I believe that we’re all an inextricable part of this grand masterpiece. Traveling is not the essential element in a voyage. Life is a voyage no matter where you are. Our voyage is how we perceive our surroundings, how we face our challenges, and how we come to Truth. Actually, none of us ask for this voyage called life. We’ve been thrust into it by forces greater than ourselves. So here we are. We do have some choices, though. Will we make the most of this journey or will we let it sweep us along without ever wondering, and questioning and being amazed?

Until tomorrow,

Mary

July 30, 2004March 18, 2021

Kevin McMahon, July 30, 2004

NOAA Teacher at Sea
Kevin McMahon
Onboard NOAA Ship Ronald H. Brown
July 26 – August 7, 2004

Mission: New England Air Quality Study (NEAQS)
Geographical Area: Northwest Atlantic Ocean
Date: July 30, 2004

Weather Data from the Bridge
Lat. 42 deg 37.86 N
Lon. 70 deg 12.37 W
Speed 8.6 kts
Barometer 1018.96 mb
Rel Humidity 93.16%
Temp. 18.9 C

The seas are calm. The skies have a distant haze. The New England atmosphere so common at this time of year. As is usual for the day, at 0700 we sent aloft a radiosonde, and then at 1000 an ozonesonde.

I was lucky enough to see a couple of finback whales; but unfortunately I had left my camera on my bunk, before beginning a discussion with Drew Hamilton about alternative power generation. Many of the scientists lead very diverse lives. Drew has a house in Seattle and wants to get off the electrical grid. He has worked for NOAA for 25 years and has seen much of the world. Thirty years ago he started out at the University of Miami, never in a thousand years dreaming he’d be involved in the kind of research he’s doing.

Ever hear of di-methyl sulfide DMS? As chemistry teacher I’d heard the name but never understood its significance to the atmospheric work the scientist aboard the ship are undertaking. It turns out that di-methyl sulfide is produced by plankton and is part of a planktons waste process. DMS is one of the major contributors of atmospheric sulfur. Overly high levels in the atmosphere can act as a reflective unit not allowing enough sunlight through our atmosphere. As a result, in certain areas the Earth does not receive the needed heat for some of the biological processes to take place.

Weather Data from the Bridge
Lat. 43 deg 17.84 N
Lon. 69 deg 33.83 W
Speed 9.3 kts
Barometer 1018.3 mb
Rel Humidity 86.16%
Temp. 20.65 C

1530 hours and there seems to be a flurry of activity among many of the scientist. A radiosonde is being rapidly readied to be sent aloft. It seems that the ship has reached a position somewhat east of Portland, ME and we have found a plume of ozone. The initial spike on the instrumentation showed 80-85 ppb (parts per billion) but then it jumped again to 101 ppb. This spike in the ozone was enough to request that another ozonesonde be readied and sent aloft. They have also requested a fly over by the DC3 out of Pease. Onboard the DC3 is a LIDAR (Light Radar) which measures atmospheric ozone. I am told that the cost of one ozonesonde is approximately one thousand dollars, so I assume that the readings on the instrumentation are justifying the expense. It will be interesting to see what they all have to say at the evening science meeting which is held each evening at 1930 hours.

We seemed to have found a large plume of ozone. It is as everyone, the science staff at least, had assumed. We have indeed found a large plume of ozone.

1930 hours. We are now heading in a westerly direction for Cape Elizabeth, ME.

November 15, 2003March 18, 2021

Debra Brice, November 15, 2003

NOAA Teacher at Sea
Debra Brice
Onboard R/V Roger Revelle
November 11-25, 2003

Mission: Ocean Observation
Geographical Area: Chilean Coast
Date: November 15, 2003

Data from the Bridge
1. 151700Z Nov 03
2. Position: LAT: 19-50.1’S, LONG: 085-03.3’W
3. Course: 189-T
4. Speed: 12.3 Kts
5. Distance: 295.6 NM
6. Steaming Time: 24H 00M
7. Station Time: 00H 00M
8. Fuel: 4233 GAL
9. Sky: OvrCst
10. Wind: 110-T, 09 Kts
11. Sea: 110-T, 2-3 Ft
12. Swell: 200-T, 3-5 Ft
13. Barometer: 1018.9 mb
14. Temperature: Air: 23.5 C, Sea 19.0 C
15. Equipment Status: NORMAL
16. Comments: None.

Science and Technology Log

We arrived at the Stratus Buoy at 1:30pm. We had some problems putting out the zodiac and will have to go and do a survey of the buoy up close tomorrow. Dr. Weller’s group will be calibrating the instruments on the buoy all day tomorrow and the following day they will be taking it out of the water in preparation to store it and ship it home. The new Stratus Buoy will be deployed in a couple of days. We continued to release radiosondes at 6 hour intervals. We are finished drooping surface drifters for awhile as well as ARGO floats. Dr. Weller did 2 CTD casts tonight to 4000m and we attached our styrofoam cups to the CTDs. I have attached some photos of our cups and my wig head after their trip into the abyss. We filmed a video of the cast that should be up in a couple of days.

A CTD stands for Conductivity, Temperature and Density. Sea water conducts electricity as a function of the amount of dissolved salts, in other words it will be a better conductor of an electrical current if it has a higher amount of salts dissolved in it. The density is calculated based on the salinity and the temperature. The salinity is calculated using the conductivity and temperature. Warm water is less dense than cold water and water with a higher salinity is more dense than water with a lower salinity. Evaporation removes water but leaves behind the salts and creates more dense water at the surface. The densest (heaviest) water sinks and the less dense water rises and you get stratification or layering of different water masses. The wind does cause mixing of the surface layer but this varies with wind speed and can vary in depth between 1 meter to 1500 meters in some areas. The CTD that we just took shows a very shallow mixed layer and we will be analyzing it a bit more closely later today. I have included a picture of the temperature/salinity/density plot from the CTD cast. The green line represents density, which is increasing from the surface down. The red line is salinity which is decreasing from the surface down but you can see some variations which show different water masses and some mixing. The brown is conductivity and the blue is temperature. We sent down the styrofoam cups and the wig heads as a demonstration of the effects of pressure. All of the air piled on top of us from the surface of the earth up into the stratosphere equals one atmosphere, but water is much more dense so if you go down 33 feet you are under 2 atmospheres of pressure and another atmosphere for every 33 feet. So how many atmospheres were our cups under? E-mail me (Debra.Brice@noaa.gov)and let me know your answer?

Personal Log

Long day punctuated by being on watch. Food is wonderful, the cooks are really creative and we have enjoyed all the meals. After dinner a lot of people will go into the lounge and watch DVDs or play board games. Most of us read or check e-mail. There is always something to do or sea and sometimes it is just nice to go outside and watch the sunset or the cloud shapes. At the CTD cast we had a spotlight on the water where the CTD went in and it attracted quite a group of large squid up to the surface. They were over 3 feet long and quite fast. The buoy has a group of 4 boobies that live on or near it feeding on the fish that gather around it. They will be most unhappy when we take it out but they will have a nice new one soon. Well, my watch is almost over and I am fading fast and this will be a busy day coming up…rumor has it that those styrofoam “cup of soup” cups shrink really well, hmmmm we need to do some more experiments on pressure……can we carve some pieces of packing styrofoam…..getting a bit carried away here:)

Cheers