Day 14- Holy Dianthus!
December 29th, 2008 by Adam SubhasMenu
Breakfast
- Ham and eggs
- Fruit salad
- Pancakes
Lunch
- Sloppy joes
- Fried rice
- Fish chowder
- Potato soup
- Salad bar
Dinner
- Cheese ravioli
- Garden marinara
- T-bone steak
- String beans
- Salad bar
Weather
Windspeed average: 40 knots. Wave height: 13-21 feet
Position
146° 15.20′ by 45° 24.19′
So I neglected to post yesterday, but our D. dianthus catch turned out to be massive! We had over 1,000 corals from a single collection, and a total of 3,795 corals for the whole dive! The great thing is that dianthus also seems to be more prevalent at lower depths, so this number should only go up as we sample deeper. We’re on our way to locations a little North of where we currently are, to try to minimize the impact of the massive weather that’s descended upon us – as of right now, we won’t be able to get back in the water with Jason until Thursday. Karen, our invertebrate biologist and resident of tasmania, said that a buoy capable of measuring wave height measured the maximum wave height at 27 meters – that’s an 88 foot wave!!!! Let’s hope we don’t see anything near that size during this trip… The average windspeed and wave height above are only going to get bigger in the next few days, though, and then will finally ease up after that – by Thursday, waves should be around 6-15 feet; with any luck, it will actually be on the low side and we can get Jason sampling again.
In the meantime, we’re doing some swath bathymetry work, which uses echo sounding to map the seafloor. Echo sounding with a single node gives a bearing – the latitude and longitude of the ship – and a range, calculated by the time it takes a sound beam to reflect off the seafloor and return to the ship. This time can be converted to a distance using the speed of sound in water. Our equipment is an EM-300, which consists of 135 nodes across the hull, making a fan of sound waves out from the ship. From each of the nodes, we get a range and a bearing, but this time the bearing is calculated using trigonometry. We know the angle at which the sound wave is emitted, and the range it gives us, thus allowing us to calculate the location that the beam hit the seafloor. Swath bathymetry, then, provides a very detailed image of the seafloor, detail obviously increasing with the number of nodes used. Interestingly, long before the public community had access to this technique, the U.S. Navy performed a lot of swath bathymetry in the Atlantic, mainly because seafloor bathymetry is very useful in hiding submarines from sonar and other detection mechanisms. If one knows the bathymetry to a very high resolution, however, it is very hard for an enemy submarine to escape detection. Much of this bathymetry still hasn’t been released to the public.
Unfortunately, swath bathymetry is a purely secondary objective, which means we only do it in bad weather, which means the data is often quite noisy. As soon as the nodes are exposed to the air, for instance when the ship crests a wave, the data becomes complete noise. Moreover, the heave of the ship means that the sound swath is constantly moving back and forth, and not progressing linearly. But since our only time to perform swath bathymetry is in bad weather, it’s the best we can do…
Karen, thanks for the answer to the riddle! We’ll surely get stuck on some more, so look out for another challenge!
