Storm names have moved into the Greek alphabet for the first time in my life since moving to the east coast (moved here in 2009). Didn’t even know that this was the convention for naming storms after first names have been exhausted! Moving into the Greek alphabet is a funny surf/academia crossover for me since I studied and read ancient Greek in both undergraduate and graduate school. When I teach ancient philosophy courses I always make my students learn the Greek alphabet first so that they can identify important Greek philosophical terms in our readings, which I like to write on the chalkboard in both their original and transliterated forms. Ya know words like philosophy (φιλοσοφία), episteme (ἐπιστήμη), ethics (ἠθίκα), aesthetics (αἴσθεσις), phronesis (φρονήσις), and democracy (δημοκρατία). I personally hold the opinion that Greek is the most important language for grasping the significance of words in scientific thought. I read Latin too, and it is important, but a greater majority of our technical scientific vocabulary derives from Greek. And apparently an important part of our technical east coast swell vocabulary does too! The Greek alphabet is as follows:
Alpha (Α, α) — short ‘a’ as in ‘ah’ or ‘hat’
Bēta (Β, β) — ‘b’ as we use it
Gamma (Γ,γ) — ‘g’ as we use it
Delta (Δ, δ) — ‘d’ as we use it
Epsilon (Ε, ε) — short ‘e’ as in ‘pet’ or ‘center’
Zēta (Ζ, ζ) — ‘z’ as we use it
Ēta (Η, η) — long ‘ē’ which sounds like a long ‘ā’ as in ‘ate’ or ‘hate’
Thēta (Θ, θ) — ‘th’ just as we use it
Iōta (Ι, ι) — ‘i’ as used in Romance languages, making the ‘eee’ sound as in ‘tortilla’
Kappa (Κ, κ) — ‘k’ as we use it
Lambda (Λ, λ) — ‘l’ as we use it
Mu (Μ, μ) — ‘m’ as we use it
Nu (Ν, ν) — ‘n’ as we use it
Ksi or Xi (Ξ, ξ) — ‘x’ as in ‘box’
Omikron (Ο, ο) — short ‘o’ as in ‘hot’
Pi (Π, π) — ‘p’ as we use it
Rho (Ρ, ρ) — ‘r’ as we use it
Sigma (Σ, σ or ς) — ‘s’ as we use it (the two ways of writing the lower case differentiate when it is used in a word or at the end of the word)
Tau (Τ, τ) — ‘t’ as we use it
Upsilon (Υ, υ) — classically ‘u’ as in ‘put’ but later transliterated as ‘y’ so the word ‘hypēr’ in ancient Greek (meaning ‘over’) may have been pronounced ‘hupēr’ — in modern Greek pronounced the same as iōta — ‘eee’
Phi (Φ, φ) — ‘ph’ as we use it to sound like ‘f’
Chi (Χ, χ) — not ‘x’ but rather ‘ch’ as in ‘Bach’ — kind of a hard ‘k’ sound
Psi (Ψ, ψ) — ‘ps’ which just sounds like ‘s’ as in ‘psychology’ or ‘psychotic’
Ōmēga (Ω, ω) — long ‘o’ as in ‘mote’ or ‘tote’
Alpha, Bēta, and Gamma all formed as storms, but I remember not where they ran off to. Delta was the first surfable Greek alphabetical swell to grace our shores. That one was mostly just local wind and didn’t last too long. I remember the most fun I had surfing Delta was the day it arrived. It was wild and chunky with hard winds from the ENE. And then about a week later Epsilon popped up on the radar.
Epsilon started in the ESE and slowly crept northward before turning its sights on Europe. And when I say slow I mean slloooowwww. I did a number of virtual oceanography courses during the start of Epsilon. It’s always fun to do an oceanography course on swell and wave generation and have there actually be a large, spinning, red blob to watch in the southern Atlantic. When I’d click the forecasted radar, advancing in sets of 12 hours, we would see that the storm was not changing relative position very much. It was moving slightly westward and slightly to the north, just in the tiniest increments. This lead me to believe that the fullest pulse of swell would arrive a bit later, and that the initial pulses would be quite weak, with longer, more infrequent lines.
Thursday, October 22, was the day Epsilon arrived, and it had all that first day swell hype. I had scheduled some sessions early, myself hoping to video since it would have been the first day without fog in the morning in quite a few days, and also because having seen how slow and far away the swell was moving, I wasn’t totally hyped to tire myself out in inconsistent closeouts. At first light people were pouring out of their cars, already suited up, shortboards under arm. The tide was very low, the sets were very few and far between, there were many closeouts, and it was packed to the gills. Still, there were some great waves coming through for the patient surfer. The patient surfer this day was Russell Kummer. Russ had one session left in his package and I’d been rescheduling with him for weeks, waiting for a day that was dry enough to film. He has been putting a ton of work in on his own, and this seemed like the day to get the last one done. Russ had an epic session. He was really patient for the sets and dealt with the crowd superlatively, letting everyone else fight and froth over closeouts, leaving himself out the back in position for the one peeler that would roll through every 5 minutes or so. We were working on him figuring out how to time and execute cutbacks and floaters — seeing the section ahead of time and getting the back foot sufficiently over the fin cluster to pivot the board around and back into the pocket. In general timing the move early and finding the fins are the keys to doing maneuvers in surfing. There are other nuances like hand placement and the amount of pressure to apply to the tail per the move, but these are secondary to understanding the wave in such a way that you see the section before you get there — this gives you enough time to prepare yourself to execute or at least attempt the maneuver. It is also generally better to start with horizontal maneuvers like cutbacks, floaters, and simple end section taps because they are founded upon finding the mid to high, fast line of the wave where you need less bodily technique to gain the requisite speed for the maneuver to be effective. Many newer surfers make the mistake of going too far to the bottom and trying to do a bottom turn-top turn combo without yet understanding whether or not the wave will allow it. You typically see people try this and burn all their speed at the bottom and either the wave rolls off without them or when they make it back up the face the wave kind of dies because it never had enough face to do such a turn in the first place.