Cold Day, Cold Feet
January 2, 2018
Day 90
Noon Position: 46 32S 35 05E
Course(t)/Speed(kts): ENE 5
Wind(t/tws): SWxW 20 – 27
Sea(t/ft): W 7
Sky: Squalls, one after the other with hail
10ths Cloud Cover: 5
Bar(mb): 1011, rising
Cabin Temp(f): 54 (48 when I woke)
Water Temp(f): 47
Relative Humidity(%): 70
Sail: #1 free to port, #2 poled out, broad reach.
Noon-to-Noon Miles Made Good (nm): 130
Miles since departure: 12,302
Avg. Miles/Day: 137
Days since Cape Horn: 33
Miles since Cape Horn: 4,657
Avg. Miles/Day: 141
Longitude Degrees Made Good (degrees minutes): 3 07
Longitude Miles Made Good (at Lat 46S): 127
Total Longitude Made Good Since Cape Horn (degrees minutes): 102 05
I can’t believe I’ve been away from my wife for 90 days. I doubt we’ve been apart this long since our first date.
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Poor day for mileage. Wind went soft but squally overnight, and that has not improved between sunup and this writing.
A frigid airmass is moving through, pushing temperatures in the cabin to 48 degrees by morning, a number not seen since Cape Horn. Condensation dripped from the port lights. Squalls have been huge and heavy and unrelenting and have dominated my day. This is because they not only bring high wind but they bend it beyond what can conscientiously be ignored.
The “true” wind wants to be about WxS at 25, and this is what we get between squalls if there’s enough room. But the squall turns that wind 50 degrees S and more; gusts are to 35 and 40 with hail. As the squall departs, wind goes 15 for a painfully long time. Then the cycle repeats.
Consequently, our course is a lazy S, no matter how much time I spend at the sheets. Am cold, tired and cranky. Have barked at Monte a few times when he fails to correct with alacrity. This, I have noticed, does not have any positive effect.
Part of the issue is that I’m nervous. We’re approaching a difficult stretch of water. Prince Edward Islands (Marion) are less than a day to the east, and 600 miles further on, the Crozets. As you may recall, it was a day’s sailing past the Crozets where Mo fell off a wave and stove in a widow in seas that were breaking for a hundred feet.
What makes this difficult water is a guess. The sea floor rises here, creating a high plateau for the islands to sit upon. Could it be that this generates upwelling which adds to the surface turbulence? Where we were knocked down was well past the Crozets and in deep water again. Does the plateau act like a big boulder in a vast sea, producing a return current in its wake? All unknown. The force of the sea is not unknown.
Arriving in the area with us are two lows, one with strong NW winds day after tomorrow and a full rotator low (NW, W, SW winds) a day later. I am usure how to handle these. Should I stay N of the Crozets in lighter winds but shallower water or stay to the S where water is deeper but winds will be stronger? Currently I’m edging N (at the behest of the squalls) with the intention of going over the top of Prince Edward. The coming northerlies will likely drive me south and just below the Crozets. That’s how things look at the moment.
Cold day … and cold feet. Nothing to do but press on and sail as smartly as possible.
time again to heat the oven?? warm up!
I know now why we haven’t heard from Monte in a while. You yell at him and he won’t talk. Who else is there to keep you company?
Hopefully you have some good books/audio books to keep you busy I have a large collection of audio books on my laptop, along with ham radio, amateur radio, that is a big entertainment solution . During my last transatlantic passage I made over 7,000 contacts. Often propagation allowed me to check into the maritime mobile net. Hey you could study the license material and get your FCC call when you’re back home I’d be glad to help if there is a way to electronically get the materials to you
Dave W8DO
Sailboat Calypso
Randall- for over a year this issue over the area around the Crozets has piqued my interest and I have been tracking the ocean dynamics and following your second attempt. On the east coast we are very sensitive to the effect of the Atlantic’s Gulf Stream on waves and weather.
The answer may lie in the merging of two main Summer current streams. The tail end of Angulhas running ESE has warmer water than the West Wind Drift running E to ENE. The Angulhas produces a lot of eddies on its southern edge that confuse the seas with a predominant wave pattern from the SW. Add to that the falloff of ocean depths which probably magnifies the eddies further. The ocean temperature gradients on maps in the area around the Crozets are unusually tighter than elsewhere in the southern Indian Ocean and I have been noticing that the wave height is larger along a band on the Southern edge of the Angulhas there.
Continued wishes of fair winds and seas through a very confused area of the ocean.
SkipC34
Interesting post, Michael Scipione. Thanks for it.