NOAA Ocean Service – Page 4 – NOAA Teacher at Sea Blog

June 8, 2015August 21, 2021

Bill Henske, Introduction, June 8, 2015

NOAA Teacher at Sea
Bill Henske
Onboard NOAA Ship Nancy Foster
June 14 – June 26, 2015

Mission: Coral Reef Condition Assessment, Coral Reef Mapping, and Fisheries Acoustics Characterizations
Geographical area of cruise: Florida Keys National Marine Sanctuary
Date: June 8, 2015

Personal Log

This is a picture of me in the St. Francis Mountains of southeast Missouri doing planning for a student backpacking trip. — This is a picture of me in the St. Francis Mountains of southeast Missouri doing planning for our middle school summer field study class.

As a middle school teacher, I often think about the experiences I had through my education that brought me to where I am now – what led to my passion for science and exploration. Giving students experiences, experts, and opportunities are essential to promoting a lifelong love of learning. When I learned about the Teacher at Sea program with the National Oceanic and Atmospheric Administration (NOAA) I eagerly applied. This is a tremendous opportunity to grow in my capacity as a science teacher, role model, and colleague. Best of all, it would be an adventure where I would learn lots of new things!

Teacher at Sea bling will come in handy on this June's cruise through the Florida Keys National Marine Sanctuary — Teacher at Sea bling will come in handy on this June’s cruise through the Florida Keys National Marine Sanctuary

I am very lucky to teach and learn at Maplewood Richmond Heights Middle School in a small, but diverse school district just outside of St. Louis, Missouri. We have a wonderful program of expeditionary learning at our public school. Our classrooms go from the watershed of our neighborhood, to the Mississippi valley, to the Appalachian Mountains, to the Gulf of Mexico. Through expeditionary learning, we can give students many similar experiences that led us teachers to enter STEM fields. Through field experiences and connections to scientists, students have opportunities to explore their interests and ignite passions.

This is a photo from 1993 when a friend and I canoed from college in Wisconsin to my home in St. Louis.

One of the important lessons we learn at our school from our study of watersheds during our 7th and 8th grade years is that we are really one giant watershed. The motto that “We all live downstream” is not just a metaphor for the way that our actions have consequences. “We all live downstream” is also very literal. My school community exists in the largest drainage area of North America, the Mississippi River. Our collective actions, whether they are positive or negative, have quantifiable effects downstream.

The interconnected systems of the hydrosphere, geosphere, and atmosphere also connect all of us humans. Because these resources are “free”, they have gone a long time through Western history without the respect of economic value. Students across our country are confronted with the sad statistics of environmental decline. They are bombarded with figures and facts about the negative trend in marine ecosystems. What truly drives my and many other teacher’s passion is the opportunity to provide the next generation with the hope of science and research. These tools will help us define problems and propose solutions that can stop or even reverse the situation.

This June I will be joining the crew of NOAA Ship Nancy Foster. We will be cruising the Florida Keys National Marine Sanctuary and the Dry Tortugas region where NOAA scientists will conduct fish sampling and acoustic tagging in order to determine the connectivity of fish populations between the various geographic entities. This essential work will help determine the fragmentation or cohesiveness of different populations of marine organisms as habitat is protected but in fragments. It would be interesting to incorporate this information and the techniques used as we set up our yearly pond study back in Missouri. Do fish move from one side of the pond to the other?

On this cruise we will also be deploying and installing the Integrated Tracking of Aquatic Animals in the Gulf of Mexico (iTag) array network. This system will help monitor the movement of marine organisms to determine larger scale movement of different populations and species. I can see this project leading to classroom lessons on population biology, genetics, and even speciation. The complexity of interactions between hundreds of species and dozens of distinct populations is truly astounding. Our scientists policy makers are often asked to distill this complexity down to a harvest number or population level. I want to bring back to my students the important role science has in, not only explaining the world around us but, shaping our future and helping develop or maintain the world we want.

Area of June NOAA cruise on the Nancy Foster — Area of June 2015 NOAA cruise on the Nancy Foster

I am so excited to be a part of the Teacher at Sea program and cannot wait to share my work and experiences with my students and school community. Every year we take our 8th grade class to the Dauphin Island Sea Lab where we study the marine science that others have discovered. This August, when I go back to the regular classroom, I will be one of the folks who helped make those discoveries!

As I finish this entry, I am thinking about how the coral, sponges, and mollusks of the Gulf will soon be filtering through the water that we floated through last week on the 11 Point River, here in Missouri. The water flows so easily and generously from the ground that an unfortunate majority here take its presence for granted. The water carried little bits of all of us, a connection, as it traveled its thousand plus miles to the ocean. On Saturday, June 14, I cycle myself through the atmosphere and hydrosphere to begin my adventure as a Teacher at Sea. Check back regularly for updates on our mission aboard the Nancy Foster and a taste of life on a research vessel.

My students and I became part of the watershed this past week, floating towards the sea along Greer Spring Branch in southern Missouri.

My students and I found a great way to cool off last week in Missouri. How long can you stand the 55º F spring water?

May 19, 2015August 21, 2021

Michael Wing: The Ocean Is Our Front Yard, May 20, 2015

NOAA Teacher at Sea
Michael Wing
Aboard R/V Fulmar
July 17 – 26, 2015

Mission: Applied California Current Ecosystem Studies Survey
Geographical Area: Northern California coast
Date: May 9, 2015

Science and Technology Log

If you live in the San Francisco Bay area, you’ve seen our “front yard” many times. You have looked west while driving across the Golden Gate Bridge, walked on a beach and faced into the wind, maybe even gone on a whale watching trip. How well do we know it? Besides the fog and wind, the whales and waves, what’s out there? After living here for two decades, I’m going to find out.

What's it like out there? — What’s it like out there?

The National Oceanic and Atmospheric Administration (NOAA) is an agency of the federal government. They’re the people who run the National Weather Service, among other things. They also do oceanographic research, and through their Teacher at Sea Program they place teachers on oceanographic ships. I am one of those fortunate teachers.

I work at Sir Francis Drake High School in San Anselmo, California. Lots of NOAA Teachers at Sea get on an airplane, fly to a distant city, board a big ship and cruise hundreds of miles out to sea; but my experience will be very local. I will never be more than about fifty miles from my house, as the gull flies. In fact, Sir Francis Drake High School is the closest major school to the Cordell Bank National Marine Sanctuary, where a lot of my time will be spent. I will also be working the waters of the Gulf of the Farallones National Marine Sanctuary. A marine sanctuary is sort of like a national park that is underwater.

The cruise I will be on is a routine one; part of a scientific program called the Applied California Current Ecosystem Studies Survey (ACCESS). The California Current is a cold, south-running current; part of a global circulation pattern called the North Pacific Gyre. Upwelling of deep ocean water keeps it fertile. There used to be very productive commercial fishing here, before we caught too many fish in the 20^th century. There are still lots of plankton, birds, and marine mammals. The ACCESS cruises happen three or four times each year. We sample, count and/or measure seawater temperature and salinity, plankton, krill, birds and whales and other marine mammals. This way we’ll know the ecological health of our front yard.

The boat I will work on is specially designed for this environment. NOAA has oceanographic vessels hundreds of feet long for offshore studies, but I will be on the R/V Fulmar, an aluminum-hulled catamaran only 67 feet long. She is technically a “small boat” and not a ship at all. She is fast and stable and six people can sleep on board, as I will. “R/V” stands for “Research Vessel.” A fulmar is a seabird that looks like a stocky gull. It spends nearly all of its life at sea. Northern Fulmars fish in the waters of the Cordell Bank and Gulf of the Farallones National Marine Sanctuaries. A catamaran is a boat with two side-by-side hulls instead of one. My jobs will include standing watches, doing science, housekeeping chores and keeping this log.

Personal Log

What do I hope to get out of this? We do a plankton lab at my school, but it is very basic. I should be more of a plankton expert after this experience. I have been interested in the Cordell Bank National Marine Sanctuary ever since Drake High became a NOAA Ocean Guardian School last year. We picked up hundreds of pounds of marine plastic debris on the beaches of the Point Reyes National Seashore and analyzed where it comes from. A lot of it is related to commercial crabbing and fishing and international shipping. Also, I and my students read flipper tags on northern elephant seals for the National Park Service, and our seals swim though these waters. So, I’ll keep an eye out for floating plastic and elephant seals.

Really, though, I can’t yet know what this experience will lead to. Serendipity is a guiding principle for most scientists; the word implies luck, chance, surprise, and the wisdom to respond appropriately to the unexpected. It means spotting opportunities and following up on them. Since I’m so local, maybe there will be a way to get a new collaboration going with NOAA. Maybe just being in a new environment with new people will make me think outside of my daily grind. All of my best ideas have come to me while traveling.

Unlike practically every other teacher in the world, I have the same students two years in a row. So if you are one of my wonderful ninth graders now, you will be one of my wonderful tenth graders when I come back from this experience. So, to my wonderful ninth graders now (and ninth-graders-to-be): Follow this blog in July! Post a comment, question, or idea. We’re going to follow up in the fall.

Did you know that Sir Francis Drake missed discovering the Golden Gate and San Francisco Bay when he sailed these waters in 1579? (The “Golden Gate” is the channel of water that the bridge crosses over; there was a Golden Gate long before there was a bridge.) We shouldn’t criticize him too harshly for that because the Spanish sailed past the Golden Gate every year for 250 years without seeing it or discovering the bay! Apparently, it doesn’t look like much from out at sea.

October 16, 2014August 21, 2021

Lauren Wilmoth: Strange Sea Creatures, October 16, 2014

NOAA Teacher at Sea
Lauren Wilmoth
Aboard NOAA Ship Rainier
October 4 – 17, 2014

Mission: Hydrographic Survey
Geographical area of cruise: Kodiak Island, Alaska
Date: Friday, October 16, 2014

Weather Data from the Bridge
Air Temperature: 7.32 °C
Wind Speed: 9.2 knots
Latitude: 57°44.179′ N
Longitude: 152°27.987′ W

Science and Technology Log

ENS Steve Wall collecting a bottom sample.

Wednesday, I went on a launch to do bottom sampling and cross lines. Wednesday was our last day of data acquisition, so the motto on the POD (Plan of the Day) was “LEAVE NO HOLIDAYS! If in doubt, ping it again!” Bottom sampling is pretty straight forward. We drive to designated locations and drop a device that looks a little like a dog poop scooper down into the water after attaching it to a wench. The device has a mechanism that holds the mouth of it open until it is jarred from hitting the bottom. When it hits the bottom, it snaps closed and hopefully snatches up some of the sediment from the bottom. Then, we reel it up with the wench and see what’s inside.

We took 10 bottom samples and most were the same. We had a fine brown sand in most samples. Some samples contained bits of shell, so we documented when that was the case. At one location, we tried for samples three times and every time, we got just water. This happens sometimes if the sea floor is rocky and the device can’t pick up the rocks. If you try three times and get no definitive answer, you label the sample as unknown. Two times we got critters in our samples. One critter we found was an amphipod most likely. The second critter was shrimp/krill-like, but I don’t know for sure. Cross lines are just collecting sonar data in lines that run parallel to the previous data lines. This gives us a better image and checks the data.

TeacheratSea 008 (8) — Survey Tech Christie and Me on our bottom sampling launch.

Unknown shrimp/krill critter from bottom sample.

Thursday, we closed out the tidal station at Terror Bay. This entailed doing staff observations, a tidal gauge leveling check, and then break down everything including completing a dive to remove the orifice. Since I have already taken part in a tidal gauge leveling check, I was assigned to the staff observations and dive party. As I mentioned in an earlier post, for staff observations you just record the level of the water by reading a staff every six minutes for three hours. We did this while on a boat, because the tide was pretty high when we got started, so we wouldn’t be able to read the staff if we were on shore. Again, the reason we do staff observations is so we can compare our results to what the tidal gauge is recording to make sure the tidal gauge is and has been working properly.

While doing staff observations, I saw a small jellyfish looking creature, but it was different. It had bilateral symmetry instead of radial symmetry. Bilateral symmetry is what we have, where one side is more or less the same as the other side. Jellyfish have radial symmetry which means instead of just one possible place you could cut to make two side that are the same, there are multiple places you can cut to make it the same on each side. Also, the critter was moving by flopping its body from side to side which is nothing like a jellyfish. I had to figure out what this was! In between our observations, Jeff, the coxswain, maneuvered the boat so I could scoop this guy into a cup. Once we finished our staff observations, we headed to the ship. I asked around and Adam (the FOO) identified my creature. It’s a hooded nudibranch (Melibe leonina). Nudibranches are sea slugs that come in a beautiful variety of colors and shapes.

ENS Wood and ENS DeCastro diving for the orifice.

After a quick return to the ship, we headed back out with a dive team to remove the orifice from underwater. Quick reminder: the orifice was basically a metal tube that air bubbles are pushed out of. The amount of pressure needed to push out the air bubbles is what tells us the depth of the water. Anyways, the water was crystal clear, so it was really neat, because we could see the divers removing the orifice and orifice tubing. Also, you could see all sorts of jellyfish and sea stars. At this point, I released the hooded nudibranch back where I got him from.

Just as we were wrapping up with everything. The master diver Katrina asked another diver Chris if he was alright, because he was just floating on his back in the water. He didn’t respond. It’s another drill! One person called it in on the radio, one of the divers hopped back in the water and checked his vitals, and another person grabbed the backboard. I helped clear the way to pull Chris on board using the backboard, strap him down with the straps, and pull out the oxygen mask. We got him back to the ship where the drill continued and the medical officer took over. It was exciting and fun to take part in this drill. This was a very unexpected drill for many people, and they acted so professional that I am sure if a real emergency occurred, they would be prepared.

Personal Log

Sadly, this was most likely my last adventure for this trip, because I fly out tomorrow afternoon. This trip has really been a one-of-a-kind experience. I have learned and have a great appreciation for what it takes to make a quality nautical chart. I am excited about bringing all that the Rainier and her crew have taught me back to the classroom to illustrate to students the importance of and the excitement involved in doing science and scientific research. Thank you so much to everyone on board Rainier for keeping me safe, helping me learn, keeping me well fed, and making my adventure awesome! Also, thank you to all those people in charge of the NOAA Teacher at Sea program who arranged my travel, published my blogs, provided me training, and allowed me to take part in this phenomenal program. Lastly, thank you to my students, family, and friends for reading my blog, participating in my polls, and asking great questions.

Did You Know?

1 knot is one nautical mile per hour which is equal to approximately 1.151 miles per hour.

Challenge:

Can you figure out what my unknown shrimp/krill critter is?

October 15, 2014August 21, 2021

Lauren Wilmoth: “Wreckish looking rock?” October 15, 2014

NOAA Teacher at Sea
Lauren Wilmoth
Aboard NOAA Ship Rainier
October 4 – 17, 2014

Mission: Hydrographic Survey
Geographical area of cruise: Kodiak Island, Alaska
Date: Wednesday, October 15th, 2014

Weather Data from the Bridge
Air Temperature: 4.4 °C
Wind Speed: 5 knots
Latitude: 57°56.9′ N
Longitude: 153°05.8′ W

Science and Technology Log

Thank you all for the comments you all have made. It helps me decide what direction to go in for my next post. One question asked, “How long does it take to map a certain area of sea floor?” That answer, as I responded, is that it depends on a number of factors including, but not limited to, how deep the water is and how flat the floor is in that area.

To make things easier, the crew uses an Excel spreadsheet with mathematical equations already built-in to determine the approximate amount of time it will take to complete an area. That answer is a bit abstract though. I wanted an answer that I could wrap my head around. The area that we are currently surveying is approximately 25 sq nautical miles, and it will take an estimated 10 days to complete the surveying of this area not including a couple of days for setting up tidal stations. To put this in perspective, Jefferson City, TN is approximately 4.077 sq nautical miles. So the area we are currently surveying is more than 6 times bigger than Jefferson City! We can do a little math to determine it would take about 2 days to survey an area the size of Jefferson City, TN assuming the features are similar to those of the area we are currently surveying.

Try to do the math yourself! Were you able to figure out how I got 2 or 3 days?

Since we’re talking numbers, Rainier surveyed an area one half the size of Puerto Rico in 2012 and 2013! We can also look at linear miles. Linear miles is the distance they traveled while surveying. It takes into account all of the lines the ship has completed. In 2012 and 2013, Rainier surveyed the same amount of linear nautical miles that it would take to go from Newport, Oregon to the South Pole Station and back!

Area we are currently surveying. — Area we are currently surveying (outlined in red) with some depth data we have collected.

Casting a CTD (Conductivity, Temperature, and Depth) gauge.

Monday, I went on a launch to collect sonar data. This is my first time to collect sonar data since I started this journey. Before we could get started, we had to cast a CTD (Conductivity, Temperature and Depth) instrument. Sound travels a different velocities in water depending on the salinity, temperature, and pressure (depth), so this instrument is slowly cast down from the boat and measures all of these aspects on its way to the ocean floor. Sound travels faster when there is higher salinity, temperature, and pressure. These factors can vary greatly from place to place and season to season.

Imagine how it might be different in the summertime versus the winter. In the summertime, the snow will be melting from the mountains and glaciers causing a increase in the amount of freshwater. Freshwater is less dense than saltwater, so it mainly stays on top. Also, that glacial runoff is often much colder than the water lower in the water column. Knowing all of this, where do you think sound will travel faster in the summertime? In the top layer of water or a lower layer of water? Now you understand why it is so important to cast a CTD to make sure that our sonar data is accurate. To learn more about how sound travels in water, click here.

TeacheratSea 033 (5) — I’m driving the boat.

After casting our CTD, we spent the day running the sonar up and down and up and down the areas that needed to be surveyed. Again, this is a little like mowing the lawn. At one point, I was on bow watch. On bow watch, you sit at the front of the boat and look out for hazards. Since this area hasn’t been surveyed since before 1939, it is possible that there could be hazards that are not charted. Also, I worked down in the cabin of the boat with the data acquisition/sonar tuning. Some important things to do below deck including communicating the plan of attack with the coxswain (boat driver), activating the sonar, and adjusting the sonar for the correct depth. I helped adjust the range of the sonar which basically tells the sonar how long to listen. If you are in deeper water, you want the sonar to listen longer, because it takes more time for the ping to come back. I also adjusted the power which controls how loud the sound ping is. Again, if you are surveying a deeper area, you might want your ping to be a little louder.

Tuesday, I helped Survey Tech Christie Rieser and Physical Scientist Fernando Ortiz with night processing. When the launches come back after acquiring sonar data, someone has to make all that data make sense and apply it to the charts, so we can determine what needs to be completed the following day. Making sense of the data is what night processing is all about. First, we converted the raw data into a form that the program for charting (CARIS) can understand. The computer does the converting, but we have to tell it to do so. Then, we apply all of the correctors that I spoke about in a previous blog in the following order: POS/MV (Position and Orientation Systems for Marine Vessels) corrector, Tides corrector, and CTD (Conductivity, Temperature, and Depth) corrector. POS/MV corrects for the rocking of the boat. For the tides corrector, we use predicted tides for now, and once all the data is collected from our tidal stations, we will add that in as well. Finally, the CTD corrects for the change in sound velocity due to differences in the water as I discussed above.

After applying all of the correctors, we have the computer use an algorithm (basically a complicated formula) to determine, based on the data, where the sea floor is. Basically, when you are collecting sonar data there is always going to be some noise (random data that is meaningless) due to reflection, refraction, kelp, fish, and even the sound from the boat. The algorithm is usually able to recognize this noise and doesn’t include it when calculating the location of the seafloor. The last step is manually cleaning the data. This is where you hide the noise, so you can get a better view of the ocean floor. Also, when you are cleaning, you are double checking the algorithm in a way, because some things that are easy for a human to distinguish as noise may have thrown off the algorithm a bit, so you can manually correct for that. Cleaning the data took the longest amount of time. It took a couple of hours. While processing the data, we did notice a possible ship wreck, but the data we have isn’t detailed enough to say whether it’s a shipwreck or a rock. Senior Tech Jackson noted in the acquisition log that it was “A wreckish looking rock or a rockish looking wreck.” We are going to have the launches go over that area several more times today to get a more clear picture of is going on at that spot.

H12662_DN195_2804 This is an example of noisy data. In this case, the noise was so great that the algorithm thought the seafloor went down 100 extra meters. Manually cleaning the data can adjust for this so our end product is accurate. The actual seafloor in this case is the relatively straight line at about 100 meters depth. — This is an example of noisy data. In this case, the noise was so great that the algorithm thought the seafloor went down 100 extra meters. Manually cleaning the data can adjust for this so our end product is accurate. The actual seafloor in this case is the relatively straight line at about 100 meters depth.

Personal Log

Monday was the most spectacular day for wildlife viewing! First, I saw a bald eagle. Then, I saw more sea otters. The most amazing experience of my trip so far happened next. Orcas were swimming all around us. They breached (came up for air) less than 6 feet from the boat. They were so beautiful! I got some good pictures, too! As if that wasn’t good enough, we also saw another type of whale from far away. I could see the blow (spray) from the whale and a dorsal fin, but I am not sure if it is was a Humpback Whale or a Fin Whale. Too cool!

Did You Know?

Killer whales are technically dolphins, because they are more closely related to other dolphins than they are to whales.

October 12, 2014August 21, 2021

Lauren Wilmoth: Shore Party, October 12, 2014

NOAA Teacher at Sea
Lauren Wilmoth
Aboard NOAA Ship Rainier
October 4 – 17, 2014

Mission: Hydrographic Survey
Geographical area of cruise: Kodiak Island, Alaska
Date: Sunday, October 12, 2014

Weather Data from the Bridge
Air Temperature: 1.92 °C
Wind Speed: 13 knots
Latitude: 58°00.411′ N
Longitude: 153°10.035′ W

Science and Technology Log

The top part of a tidal station. In the plastic box is a computer and the pressure gauge.

In a previous post, I discussed how the multibeam sonar data has to be corrected for tides, but where does the tide data come from? Yesterday, I learned first hand where this data comes from. Rainier‘s crew sets up temporary tidal stations that monitor the tides continuously for at least 30 days. If we were working somewhere where there were permanent tidal station, we could just use the data from the permanent stations. For example, the Atlantic coast has many more permanent tidal stations than the places in Alaska where Rainier works. Since we are in a more remote area, these gauges must be installed before sonar data is collected in an area.

We are returning to an area where the majority of the hydrographic data was collected several weeks ago, so I didn’t get to see a full tidal station install, but I did go with the shore party to determine whether or not the tidal station was still in working condition.

A tidal station consists of several parts: 1) an underwater orifice 2) tube running nitrogen gas to the orifice 3) a nitrogen tank 4) a tidal gauge (pressure sensor and computer to record data) 5) solar panel 6) a satellite antennae.

Let me explain how these things work. Nitrogen is bubbled into the orifice through the tubing. The pressure gauge that is located on land in a weatherproof box with a laptop computer is recording how much pressure is required to push those bubbles out of the orifice. Basically, if the water is deep (high tide) there will be greater water pressure, so it will require more pressure to push bubbles out of the orifice. Using this pressure measurement, we can determine the level of the tide. Additionally, the solar panel powers the whole setup, and the satellite antennae transmits the data to the ship. For more information on the particulars of tidal stations click here

Tidal station set-up. Drawing courtesy of Katrina Poremba.

Rainier is in good hands. — *Rainier* is in good hands.

The tidal station in Terror Bay did need some repairs. The orifice was still in place which is very good news, because reinstalling the orifice would have required divers. However, the tidal gauge needed to be replaced. Some of the equipment was submerged at one point and a bear pooped on the solar panel. No joke!

After the tidal gauge was installed, we had to confirm that the orifice hadn’t shifted. To do this, we take manual readings of the tide using a staff that the crew set-up during installation of the tidal station. To take manual (staff) observations, you just measure and record the water level every 6 minutes. If the manual (staff) observations match the readings we are getting from the tidal gauge, then the orifice is likely in the correct spot.

Just to be sure that the staff didn’t shift, we also use a level to compare the location of the staff to the location of 5 known tidal benchmarks that were set when the station was being set up as well. As you can see, accounting for the tides is a complex process with multiple checks and double checks in place. These checks may seem a bit much, but a lot of shifting and movement can occur in these areas. Plus, these checks are the best way to ensure our data is accurate.

Micki and Adam setting up the staff, so they can make sure it hasn't moved. — ENS Micki and LTJG Adam setting up the staff, so the surveyor can make sure it hasn’t moved.

Mussels and barnacles on a rock in Terror Bay.

Leveling to ensure staff and tidal benchmarks haven't moved. — Leveling to ensure staff and tidal benchmarks haven’t moved.

Today, I went to shore again to a different area called Driver Bay. This time we were taking down the equipment from a tidal gauge, because Rainier is quickly approaching the end of her 2014 season. Driver Bay is a beautiful location, but the weather wasn’t quite as pretty as the location. It snowed on our way in! Junior Officer Micki Ream who has been doing this for a few years said this was the first time she’d experienced snow while going on a tidal launch. Because of the wave action, this is a very dynamic area which means it changes a lot.

In fact, the staff that had been originally used to manually measure tides was completely gone, so we just needed to take down the tidal gauges, satellite antenna, solar panels, and orifice tubing. The orifice itself was to be removed later by a dive team, because it is under water. After completing the tidal gauge breakdown, we hopped back on the boat for a very bumpy ride back to Rainier. I got a little water in my boots when I was hopping back aboard the smaller boat, but it wasn’t as cold as I had expected. Fortunately, the boat has washers and driers. It looks like tonight will be laundry night.

Personal Log

The food here is great! Last night we had spaghetti and meatballs, and they were phenomenal. Every morning I get eggs cooked to order. On top of that, there is dessert for every lunch and dinner! Don’t judge me if I come back 10 lbs. heavier. Another cool perk is that we get to see movies that are still in the theaters! They order two movies a night that we can choose from. Lastly, I haven’t gotten seasick. Our transit from Seward to Kodiak was wavy, but I don’t think it was as bad as we were expecting. The motion sickness medicines did the trick, because I didn’t feel sick at all.

Did You Know?

NOAA (National Oceanic and Atmospheric Administration) contains several different branches including the National Weather Service which is responsible for forecasting weather and issuing weather alerts.

Animal Spotting

There are sea otters everywhere!

Sea otter (Enhydra lutris) sighting. — Sea otter (*Enhydra lutris)* sighting.