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Challenger 1’s Sailing Away…

Morning everyone,

Over this past weekend, Challenger 1 has soarded through the Atlantic, travelling nearly 96km (~60miles). For the past two weeks, around the time we were halfway past Ireland, the currents started really aiding us. Manipulating through the Eastern side of clockwise rotating eddys with strong Southern- Southeasterly currents boosted us through the ocean. We are currently almost halfway past France and more than halfway to the Azores, where we may get Challenger 1 recharged and cleaned off, we are not quite certain yet.

Also, the team decided to move the waypoint a little ways to the West after the next few surfacings. It’s not going to be moved immediately because we still want to take advantage of the beneficial currents in the current path with the current waypoint.

-Oliver

The end of the first chapter…

 

“This one is neither the end, nor even the beginning of the end… but the end of the beginning”… (W. Churchill)

Hey guys…

Silbo is ending the first chapter (30 %) of his great history … He has flown 1500 km at 0.3 m/s (1.1 km/h) during 57 days. He is crossing right now the green and magic western coast of Ireland.

Figure 1.- Silbo crossing (23 jun-19 aug 2011).

During these 1500 kms we have tried to fly the eastern side of the warm eddies. When we plot the synoptic profile of salinity and Temperature clockwise warm cores appear clearly above 400 m (in the epipelagic domain).

 

Figure 2.- Silbo profiles of Temperature and Salinity (23 jun-19 aug 2011).

Now, he is heading the main Gulf Stream branch located on 40s parallels. The first change that we would observe on this second chapter are poorer oligotrophic waters, at warmer SSTs and higher salinities.  However, the most important remark is that we left the thermohaline branch of the gulf stream flowing N (to Iceland) and we would begin to observe currents flowing E (to the French-Spaniard Gulf of Biscaine) and SE (Madeira-Canary islands).  It can be observed in the northern border of the main gulf stream branch in the map of salinity (figure 5). They are all warm eddies formed in the border resulting of an eastern flow of the general current path.

Figure 3.- Chl a field MODIS (19 aug 2011).

Figure 4.- SST field MODIS (19 aug 2011).

Figure 5.- Salinity field (19 aug 2011).

However, during the last week Silbo has reduced his speed. We expected intense current flowing SE-S and all the model (the last post) forecasted that silbo would cross the eastern side of warm eddies at higer speeds than observed on the ground.

Figure 6.- SSHa field (19 aug 2011).

Figure 7.- Current field (17-18-19 aug 2011).

The explanation to this extrange behaviour of this current fields was suggested in the last post, and, two days later, confirmed by Silbo on the ground. Storms (22 in 57 days) become stronger and more active at this latitudes (SST increases). The first effect of  storm is a significant change on current path. Since the 23 of june we have suffered two strong inertial oscillations that turned the direction of the current 360 degrees in 14-18 hours.

We think that we are actually suffering one of this inertial perturbation as a result of our 22th and 23th respective storms crossing at Silbo Latitude domain. It could explain the incongruence of his ground true current with these obtained from global models. Daily Global Models output would not explain the hourly variation of the current speed. To report such a feature, it would be neccessary to use ROM data (Regional Ocean Model outputs). But this, are only available in the European Domain eastern 20 W (we are at 24.5 W).

Figure 8.- Inertial oscillation (17-18-19 aug 2011).

We would keep you updated the next days.

have a nice weekend

Antonio Ramos & Nilsen Strandskov

 

Arms of the Gulf Stream

Hey All!

Challenger weaving its way through the eddy solar system

 

As Challenger 1 continues to work its way south along the eastern side of the second large warm eddy of the solar system and battle its way through our 22nd storm, we continue to make good progress as we are now half way to the Azores!!!  The two images above are of Sea Surface Height showing our path along the eastern side of a large eddy.  Keeping this pace, we could reach the Azores by the 2nd week in October and so if Challenger has begun feeling any effects from biological growth, we will be able to provide aid.

Storm # 22

These storms however are intensifying as we get later in the year.  As the summer months warm the North Atlantic, the strong storms we see along the Eastern Sea Board of the U.S. gain strength as they then are carried by the Jet Stream right to us!

Speaking of the warming seas, lets look at an interesting point in the temperature data from the North Atlantic.

Sea Surface Temperatur Map (Top) and Temperatures at a depth of 300m

The first image is surface temperatures while the second image is of temperature at depths of 300m.  The second image shows how deep the effects of some of the larger eddies can be seen.

Similarly, looking at the temperature profiles from Challenger since deployment, we can see the thermocline grow deeper as we passed through the wall of warm core eddies along our journey.

Finally, we see something very interesting looking at the sea surface salinity maps of the North Atlantic.  Below, we can see that we are on just the outer edge of the northern arm of the Gulf Stream.  We predict, that once we cross into the 40’s latitudes and past the edge of the Gulf Stream, we will find even stronger currents that will aid us further on our way to greatness!

Salinity Map of the North Atlantic showing the branches of the Gulf Stream

Stay tuned for more updates soon!

Nilsen & Antonio

A Few New Road Maps

Hey All!

So Challenger 1 has made considerable progress within the past few days. Since Friday, Challenger 1 has flown roughly 122km/75 miles, breaking our speed record yet again hitting 0.63 m/s!!

We harnessed the power of the clockwise flow of the Eastern-side of the eddys and are cruising. For the next few days the currents seem favorable, quickly heading in the East – Southeast direction, ever closer to our waypoint.

Today, Antonio have us a few new products that will likely help us even more on our travels.

First he gave us a new Sea Surface Height map takes the european geoid (mean surface height), and calculates the isopotential surface position and from there highlights and predicts surface anomalies.

This will give us another perspective on where the warm and cold eddies are and predicted to go to better our forecast and piloting judgements.

Next we have a new current map that shows the intensity of the vertical attribute of the currents.  So on the map below, the darker red the area, the stronger the currents are moving north, while darker blue means a southerly movement.

As the maps above show, we are still in the reaches of the strong warm eddy we had first encountered late last week that threatened to pull us back out west, but we should officially be out of its reach over the next day or so and continue on our way south.

Also with how well these warm eddies are lined up, we hope to not have to change the way point for a while as we plan to just surf the currents from the east side of one warm eddy to the next until we are out of this solar system.

We will keep everyone updated!

Nilsen , Antonio, and Oliver

 

Planet 51…

Hey guys

this mission is converting in a “planet 51- like” adventure.

Fig 1.- Planet 51.

Silbo follows flying a marine galaxy full of warm and cold core eddies. They aggregate and disagreggate conforming an incredible set of marine solar systems. We have explained that this kind of features keeps and transmits gyring momentum from eddy to eddy and stands for a long periods and keeping its rotation energy.

Fig 2.- SSHa  (3D). 12 aug 2011.

This is very important since it leaves us jumping from solar system to solar system taking advantage of those sectors where the currents move Silbo to the South (the Eastern side of the warm eddies).

It has  been the main reason that we changed the WP: First to 49 N, 19 W, and, looking our excesive drifting to East,  we moved it 4 degrees to W: 49 N, 23 W yesterday.

Right now, we are where we wanted to be: In the eastern side (24 W meridian) of a warm eddies chain between both solar system observed in the silbo domain, between the 54 N and 45 N paralels.

Fig 3.- SSHa  (3D). 12 aug 2011. The next Silbo path.

The new WP has worked fine. We have burnt our speed record (now in 0.57 m/s), and this morning, we covered our 15th  consecutive stint running > 10 km (>13 km some of them).

Fig 4.- SSHa  (3D). 12 aug 2011.

Current field has slighty changed to SW. They result of the South sector of the first warm eddy that we have just ecrossed. However, this weekend the silbo team expects to burn again the speed absolute record since we are now heading a new strong warm eddy signal with a significant SSHa gradient and the strongest South oriented currents field during this first 25 % of the mission.

Fig 5.- SSHa + TOTAL current field.

Have a nice Weeekend

Antonio Ramos, Nilsen Strandskov and Oliver Ho.

 

Success!

Hey All!

Well Challenger continues to plunge its way through the intersection of currents that lie in our area due to the overwhelming amount of eddies.  Last night we changed the way point further south as to prevent us from being pulled too far east by the warm core eddy next to us.  The changed way point successfully steered us out of its pull to the north, but for the time being we are sailing in a bit of a head current until we can break free from its control.

Even though we have lost some speed, we are predicting that we may break even our most recent high speed record of 0.57 m/s over the next couple days as the strongest southerly current we have seen to date lies only a short distance to our south.  This will launch us at high speeds southward along the eastern side of three warm core eddies before we may change direction and try and aim for the western side of a cold eddy to weave ourselves back around.  But that decision will be made for certain in the future.

Aside from our success with last nights change of way point, we have some really beautiful imagery from both our HYCOM and ULPGC models that all seem to match up fairly well (not always the case but really leaves us with a good feeling about what our plan is for the time being).

Sea Surface Height with Currents from the HYCOM model

Sea Surface Height with Currents from ULPGC model

Although the scales are different for the color on the two sea surface height images above, the correlation of the currents are the same showing the strong southerly flow.

Sea Surface Temperature with Currents from HYCOM model

Satellite Sea Surface Temperature with Current model from ULPGC

Unfortunately due to cloud cover courtesy of the storm number 20, there isn’t any temperature data for the imagery, same with chlorophyll a below.

Satellite Imagery of Chl a with Current model from ULPGC

Sea Surface Salinity with Currents from HYCOM model

As described in our post from a few days ago, when on the east side of a warm eddy, salinity, temperature and currents all tend to match up.

Sea Surface Density and Currents from HYCOM model

We will keep everyone updated over the next couple of days.  Have a great weekend everyone!

 

Nilsen & Oliver

Enter the Roaring 20’s!

Hey All,

Well Challenger is now being pummeled with his 20th storm in the 49 days since being deployed way back on June 23.

As you can see from the figure above, the presence of a strong system in the jet stream coincides with some wave activity reaching 8 ft swells, and a cloud system all in the vicinity of Challenger 1.

This storm however has not been able to slow us down as we have now had 7 consecutive segments all above 0.52 m/s!

Although it also seems that the currents are changing as we continue on our way to the south east so these speeds may not be around much longer.  As it says in the figure below, we are beginning to feel the effects of the currents moving to the north from the west side of the warm eddy to our east.  Depicted by the three lines, we can see that we have been leveling off and turning to the east because of this influence.

So we proposed a new way point of 49N 23 W to try and steer ourselves away from the eddy to our east’s influence and to try and continue to surf the eddy to our south.

If we continue on our current path, we will be dragged into this North East flow

Zooming out, we can see the next two solar systems that we will be navigating over the next two weeks.

Hopefully moving the way point to our south will be enough to put us on the right path to follow the yellow arrows down the stream of warm planets to the next system.  The new way point will be set at the next surfacing in a couple of hours, so hopefully it won’t be too late to try and change our course to catch the more southerly currents.  Tomorrow we will make sure to give everyone an update on how Challenger flying.

Nilsen, Antonio, and Oliver

-Chewie… we’ve hit Lightspeed! Celebrations, Recap & Record Smashing

‘Afternoon everyone,

Yesterday was a big day for us here at IMCS, we were honored with a visit from the Assistant Secretary of Commerce for Environmental Observation and Prediction, Dr. Kathy Sullivan and Director of the Integrated Oceans Observing System (IOOS) Dr. Zdenka Willis, along with a number of other high ranking government officials.  After a tour and discussion of the glider lab, COOL room, and the Challenger Mission (which consisted of a skype call with our partners at PLOCAN), everyone proceeded to the Alampi Room.  There, various awards were given out for Rutgers appreciation and collaboration and Dr. Sullivan even presented us with an award for the success of the Atlantic Crossing and luck on the completion of the Challenger Mission.

Scott Glenn, Zdenka Willis and Kathryn Sullivan touring the COOL room

Our friends at PLOCAN (including past students of the COOL room, Dara, Adri and Alvaro)during a skype session while our visitors were here.

But back to Challenger 1.  There has been a lot that has happened piloting wise over the past two weeks so first we would just like to do a quick re-cap.

Jumping back a bit, we were entering a new solar system, which we carved a path straight through the middle where we snaked back and forth jumping from one eddy to the next.

Moving on from there, we found a strong warm core eddy, the “warm planet” that really slowed our progress as we were dragged nearly directly to the west as we were pulled into it’s strong clockwise gyre.

This was then followed by our encounter with a “Mystery Eddy” on Sunday that again caught us off guard with its strength, reminding us that the ocean is a formidable foe that is still widely unknown and which should not be underestimated.

These were all very good learning experiences that will aid us on the remaining 75% of our journey.  Antonio pointed out after we were liberated from the allure of the mystery eddy, that when we cross the west side of a cold eddy (general counter clockwise), it seems that the currents we observed (as we crossed the past two solar systems) is going to the North- North/West direction, flowing in the same direction as the thermohaline pattern, but do not completely follow what the models say the currents should be.  However, when we fly on the eastern side of a warm eddythe currents agree with what the models predict, going East-South/East (clockwise motion) and thus opposite of the North-North/West thermohaline flow we see in this region.  The result of both of the counter currents we see is to the south, which are the currents we must ride until we find more favorable currents. This explains the trouble we were having when it came to flying to the west side of a cold eddy and our experience with the mystery eddy.

The North Atlantic Thermohaline Circulation showing the N-NW flow in our area that we have dealt with recently

So what we have to look for now, is to aim for the eastern side of the warm eddies, where we have found much better luck propulsion wise versus catching the western side of a cold eddy.  This however we think will change when we reach the Canary current, where we should find better luck on the western edge of a cold eddy.

After this break through, Monday we saw some strong currents to our south east that we thought may be ideal so we began looking into the changing of the way point for Challenger 1.

Our two options for waypoints. Yellow would be the range we followed keeping the waypoint, Green if we changed it

After much discussion, Antonio and I decided we should move our way point further east and aim for the stronger currents we saw to the south east of our position.  Below we can see the strong currents turning from east to south/east as it curves around the large red-yellow swirl to our south.

With this way point move, Challenger went from being a glider to a rocket ship as we broke our previous speed record not once, or twice, but on our past 4 segments!

The first two segments that broke our speed record

 

Previously, we were holding a record of 0.47 m/s, but on our past 4 surfacings, we blasted that away going 0.52m/s on the first two segments and the most recent two at 0.53 m/s!

Now we look to the near future to see when the next plan of action shall take place.  As the conditions are now, when Challenger gets to the vicinity of the circle drawn on the map above, we will move the way point back to the south to  try and take the most advantage of favorable currents.

As always, force, wind, sea and honor

Nilsen Strandskov, Antonio Ramos, and Oliver Ho

 

Chewie, prepare for the jump to LIGHTSPEED

Good morning all!

Just a quick update on the Challenger mission

So last night after Antonio and I conversed and changed the way point, Challenger came close to breaking its speed record for the mission by hitting 1.52 km/hr (0.42m/s)!  What contributed to this speed, was we moved the way point further east, allowing us to catch the outer edge of the east side of the warm eddy to our south.  This launched us on a south east trajectory following these new currents shown below.

 

That’s all for now, we will have another post later today

 

Nilsen

Thermal Wind

Hi all,

we are trying to estimate the heat transportation along the SILBO path. To this end we are using essentially the thermal wind equations. Thermal wind is the most fundamental and significant dynamical balance controlling the large-scale circulation of the ocean. It is a consequence of hydrostatic and geostrophic balance, and appears as variations of geostrophic vertical velocity if density varies horizontally.

At first, in order to determine the scale at which processes take place, we took Rossby Radius as our reference (10 km in our case), so the processes will be on that scale. It’s a good criteria to quantify all the mesoscale data. Every change in lower scales will be insignificance in our estimation.

After, we made an harmonic analysis, applying the Fourier Transform in order to estimate at which lengths (Δy) the changes of density gets more important for every range of depths (Δz = 10m, Figure 1). As we can see, most of the energy (90%, Figure 2) is concentrated above 100km (The red line indicates 100 km, and all the lengths at the left of this line are larger lengths). These analysis indicate that we are able to make different averaging among 10 and 100 kms in the direction of the glider path.

Figure 1

Figure 2

Finally, we applied the Thermal Wind equations with 10m as Δz and 10km as Δy (Figure 3). As we can see the variation of velocity gets higher while we get the surface. All these velocities are around 0 – 0.3 m/s in the surface along the glider path. These results seem to agree with real values.

Figure 3

Next step will be comparing these current velocities with the measured currents from the glider in order to check these results, before estimating the heat transportation combining these results with the measured temperature from glider.

Ruben & Alberto

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