Through the afternoon and evening, large-scale subsidence associated with the North Pacific High maintains a warm, dry cap aloft, adiabatically reinforcing the inversion that sits above the cool marine layer at the coast. This subsidence-capped marine boundary layer is a hallmark of the Bay Area’s summer climate, with marine stratus and fog waxing and waning as the daily wind/pressure cycle strengthens onshore flow by day, clears back toward the coast in the afternoon, and rebuilds overnight into early morning. Similar eastern-boundary-current settings show the same physics: the camanchaca/garúa of Peru–Chile under the Humboldt Current, the Namib fog sustained by the Benguela Current, and summer stratocumulus along Portugal–Morocco under the Azores High—all echo the Bay’s Gain-of-Fog across their own terrain and seas.
In spring and summer, marine stratus—often thickening into fog at the coast—regularly blankets the shoreline, especially near the Golden Gate and outer coast. Along Northern California, summer fog frequency is typically ~40–44% of hours near coastal sites. This regime is sustained by cold, upwelled waters of the California Current (about 52–55 °F / 11–13 °C in summer) that cool and stabilize the marine boundary layer, while inland heating establishes pressure gradients that draw the moist layer ashore. The cycle tends to peak overnight and toward early morning, clear back to the coast during the afternoon, and redevelop offshore in the evening, priming the next day’s return.
The San Francisco fog has shaped the city’s history and identity for centuries. Drake sailed by the entrance to San Francisco Bay in 1579, but the harbor remained undiscovered—likely concealed by summer fog and its narrow opening. Early Spanish explorers in the 18th century likewise recorded the fog as both a navigational hazard and a natural protector, cloaking the shoreline and adding to its mystique. On clearer days, those same explorers saw the jagged granite peaks rising offshore and named them Los Farallones—“the cliffs” or “claws”—for their sharp, claw-like silhouettes emerging from the fog. Over time, the fog became woven into local art, literature, and folklore, while also shaping how people live and dress outdoors. Windbreakers, gaiters, and extras combined with layering, help maintain body temperature in homeostasis with the fog and within the various microclimates that shift throughout the day, requiring adjustment as you 'shift in gear'. In recent decades, the city’s cultural embrace of this weather phenomenon has reflected not only its role in cooling summers but also how it challenges daily routines, defining San Francisco’s distinctive outdoor summer experience.
We have lived in and around the Bay Area for thousands of years, in unison with the recognizable estuarine environment of the modern San Francisco Bay, which took shape only around 10,000–11,000 years ago as rising seas after the last Ice Age flooded ancient river valleys. Life persisted in the fog-formed ecosystems of the area, following essentially the same daily patterns of summer fog that still occur today—rolling in by evening, spreading overnight, and retreating under the afternoon sun, though its frequency and inland reach have varied over time. Paleoecological studies confirm that fog has long been a crucial moisture source for coastal ecosystems. Measurements of stable isotopes in redwood growth rings show that fog-derived water contributes significantly to tree physiology during the summer dry season. These findings align with long-term observations showing that fog drip provides 20–45% of the total water budget in redwood stands, underscoring how this process has sustained both natural ecosystems and, indirectly, all who depended on them.
Late afternoon into evening, onshore winds often help low clouds/fog re-form offshore and push inland through the Golden Gate. Coverage commonly envelops western San Francisco (Sunset and Richmond) and, on many days, extends across the Bay to the East Bay shoreline and up the Berkeley/Oakland hills by evening or overnight. The inland reach ranges from just a few miles to across the Bay, depending on marine-layer depth and the pressure/wind setup that day.
During daylight, the marine layer’s inland reach is usually limited because the layer is often shallow (<~1,000 ft) by afternoon and blocked by coastal hills/ridges; meanwhile, daytime heating over land mixes and evaporates the cloud deck, driving the familiar afternoon clearing back toward the coast. The result is sharp microclimates—clear a few miles inland while thick stratus hugs the coast. East of the Oakland/Berkeley hills (crest ~1,700+ ft), regular, persistent coastal fog is uncommon; deeper layers and gap flows can still carry low clouds inland later in the day or overnight, especially through the Carquinez Strait.
At night, marine fog frequently lingers and can continue drifting farther inland—primarily through the Golden Gate—often reaching its maximum extent toward dawn, then retreating coastward through late morning to midday. North of the Gate, the canopy spreads into Marin lowlands and valleys, pooling against coastal ridges and sliding inland via the Petaluma Gap toward San Rafael and Napa. Under these overnight conditions, a stable subsidence inversion suppresses vertical mixing, allowing the deck to fill in and thicken: along the immediate coast the cloud base lowers to a few hundred feet or the surface (fog), while just inland it presents as stratus with ~800–1,200 ft ceilings. Inland reach commonly extends ~10–15 miles, and in stronger pushes 20–40 miles into Napa/Sonoma or even toward the interior via the Carquinez Strait. Laterally, the canopy can span Bay margins—from San Francisco to Oakland and down toward Mountain View—before thinning into patchy decks toward the South Bay and Delta. This nocturnal marine cover tempers overnight temperatures and moistens coastal ecosystems, shaping the region’s microclimates.
This fog-driven microclimate yields remarkably sharp temperature contrasts: coastal and near-coastal zones stay cool and cloudy while interior valleys (e.g., San Jose, Fremont, Concord) commonly run ~15–25 °F warmer—often 20 °F (≈11 °C) or more on typical summer days. These strong atmospheric and terrain-driven gradients define the Bay Area’s distinct climatic zones, steering local weather and ecology—coastal cloud cover moderates temperatures, raises humidity, and even supplies water to ecosystems such as redwood forests—while also shaping human activities from daily clothing choices to energy use.
The dense summer fog over the Bay Area isn’t merely weather—it’s the visible edge of a coupled ocean–atmosphere system: cold, upwelled water in the California Current, subsidence and onshore pressure gradients tied to the North Pacific High, gap-and-ridge topography along the coast, and the diurnal cycle of daytime solar heating and nighttime cooling. Its reach has shaped microclimates, ecosystems, and human choices, and it’s become part of the region’s cultural identity.
FOG
ENTER —
THE°NEXT
CAST —
♊︎ ☼ ⟳rb hPa
🅐 Day’s ATMP–DEWP Spread: 0.5 °F ∼
🅐 Refusal to burn off beneath the arc ∼
🅐 Lifting Condensation Level (LCL) held low, near-skimming sea ∼
🅐 Floor of fractional feelers ∼
Fog Stability Index (FSI)
FSI = 2(0.2) + 2(−16) + 30
= 0.4 − 32 + 30
= −1.6
FSI = −1.6 → Fog-forming regime: saturation below inversion.
Pacific High–capped marine layer (ML) — stable, moist, shallow.
• WTMP : 52.0 °F (sea-surface temperature)
• ATMP : 54.0 °F (air temperature)
• DEWP : 53.5 °F (dew point)
• RH : 98 % (relative humidity — near saturation)
• Pressure : 30.03 in Hg (steady; subsiding Pacific High)
• Wind Dir : NNW (325°) (coastal upwelling regime)
• Wind Spd : 17–22 kts (moderate mixing, advection strength)
• Inversion Base : ≈ 0.21 mi (≈ 1,100 ft)
• Marine Layer [ML] Depth : ≈ 0.15 mi (≈ 800 ft)
• Visibility : 0.20 mi (≈ 1,050 ft)
▼
FANES
▲
│
│
│
🜁 Fog
🜂 Ocean
🜃 Ground
│
│
│
▼
FARAN
▲
SKY. ▸ HIGHLAND. ▸ MARINE LAYER.
Indwelt—vibrating molecules and amorphous atoms,
Sun-in—
each a host of hidden crux,
shaking to the max in daytime convection—up to 0.75 mi—
kindled by superabitic street heat,
insolation fierce, hidrosis throes sensoria;
compounded to the breath—cornea to film, to pores;
rising vapor draws down the Lifting Condensation Level (LCL),
where cloud-born droplets rise, collide, and return—
eyes white-opened—cumulus breasting overhead;
bright, dry sky—pupils pight in;
a sea-breeze front’s kick to convection—surging inland—
saline-laced air,
condensation–dilation tasted:
the marine air’s snare.
⟁ veered FOG pours eastward ∼
⟁ fluidal vectoring through mirrored gradients ∼
⟁ marine-cooled sinewave in advection ∼
⟁ surge shaped by pressure gradients ∼
⟁ distant vehicle of physical law ∼
⟁ haze cycle sailed and spun—fun ∼
⟁ loop unclosed in recursion ∼
⟁drift beneath the inversion ceiling ∼
⟁wash upon the heated column ∼
⟁poria’s sky resolves in F.O.G.
▲
SEA LEVEL. ▸ LAND. ▸ OCEAN.
To the seaward Pacific—a carbonaceous-chondrite marina along the brined frontier,
Fog-in—
colder now to the apparent wind felt across sea and land,
within the MBL—Marine Boundary Layer—arranged in tiers:
The microphysical drivers—margins of transitional skins:
(Upper) the Cloud-Top Entrainment Zone (CTEZ),
situated at the boundary between the Marine Layer and the free troposphere,
inherently warmed by upper-tropospheric subsidence through adiabatic compression,
receiving short-wave solar input at the cloud top and
long-wave infrared emission rising from the sea,
with entrained dry air mixing downward toward balance at the inversion’s crown,
inducing evaporative cooling at the fog-top edge and sharpening the stability above,
gathering the moist deck into a coherent coastal stratus field, hie on coastal collect;
softening the lapse rate and lowering the effective fog-top boundary,
where the PSI layer—its temperature maintained by persistent subsident warming—
fixes the inversion base, defining the Marine Layer’s upper stop-cap plane.
(Mid-Stratus) within the mid-deck—saturated, optically dense, and weakly convecting,
droplets remain near adiabatic equilibrium, mist-ghosted into pitch;
radiative cooling at the cloud top initiates turbulent mixing,
constraining the vertical temperature gradient and limiting layer deepening,
as fog droplets emit longwave radiation efficiently at the fog-top interface,
intensifying the cooling zone and producing localized negative buoyancy;
small eddies transport moisture and liquid-water content laterally and vertically,
sustaining a well-mixed but mildly stable mid-deck in sound to up and down surround.
(Lower) at the littoral skin—diffuse and thin—
marine aerosols and sea-salt nuclei (CCN) initiate activation and condensation,
regulating exchanges of heat, moisture, and turbulent flow,
impelled by upward sensible and latent heat fluxes,
arising into the lost toll, sustaining its thermodynamic base,
as cold SSTs cool the surface air toward saturation,
preparing the fog-forming skin (LCL),
wherein sol rides the sine-sign at 64°.
The Marine Layer soon—sea suspended in the rare tonight—
inwalls the surface surge—a shallow diurnal onshore–offshore exchange loop,
drawn through a quasi-cincture of air, water, and land.
Along a coastal offshoot of the subsidence wing of the [NPH] North Pacific High,
aligned with the low-level [LLJ] regional jet—
a northwesterly wind coursing beneath the inversion’s crown;
the microclimatology—upheld: a flow firm on sinking;
unheld: a foothold fluid aground—condensed within the MBL,
stratified in motion—fog-potion #3.
June — Upper: humid at sixty;
July — Mid-stratus: near ninety;
August — Lower: escape to sea.
Secreted, stellated—one hundred;
ocean-cooled air recasting the facets,
the unseen floor, kairos-emanateth, quickening to fascinating,
visibility enfolded; and, in pass,
mired too steep at ocean mass,
deepened—by the things to do under the Pacific High.
🜁 — Cope’s Percentage — 🜄
Out it seams—ontically subsiding in ceptions of efflux and exchange-o’s.
Fast! forfend, formatted for F.O.G.—
flowing fabric forward, finding frontogenesis.
Figurae free-fabricating formulae—fogged fluctuations.
Enter its penetralia—Grith of Fog—FLTFOGMASKGRU-PAC.
Interoexteroproprionociception.
CN-V: clad in thermal order; gradated into the open,
where sidereal grain accrues.
fenced-in to microclimate’s exchange-counterchange-rechange.
A local, zonal rivage uprears—
outgassed to an early nightpiece, raised on ancient ocean,
its lineage living in intervening waves,
omnipresent in the self-mixing gas,
in a tableau-hap bearing down
to the sky’s surmise—
an omened, breathing galactic tap,
out, over, and onward.
Absorptivity draws the cooling inhale hale—
Equipoised ataraxis through obnubilation
🜁-conditioned in a radiative, steadied balance,
in motoric deliverance—U’ll seek.
All herald a renewal-of-life, reign of stacked gyres,
high-loft anticyclonic sky—the [N₂·O₂·Ar·CO₂] NP High;
low-lave anticyclonic ocean—the [H₂O] NP Gyre—
on the lie of water and of air—
made to stage, lingering, foreordained into gloam;
echoing into ubiety, impictured through the shades of sender and senter,
receivers to the ground-laying upon the pHz frequency of two oceans—10⁻¹²:
Hydrospheric and Atmospheric—the Ætions of Enterfog,
raving subsea to acclivities’ greige glare—
fogs of 58–62 °F wrung in the Trilateral Colloidilation,
capped beneath the Pacific Subsidence Inversion [PSI]—
an overtop held steady—the terra–mare–aer-charmer visage,
rolling over ridges, lapping clearer toward the heats.
◯
Sky to Street Vertical Profile
(Arranged from Highest to Lowest)
THE FIRMAMENT (Cosmic Realms)
1. Beyond observable universe
2. Observable universe boundary
3. Cosmic voids
4. Cosmic web
5. Intergalactic medium
6. Interstellar medium
7. Heliosphere
8. Interplanetary space
UPPER ATMOSPHERE (Exo- to Strat-)
9. Exosphere
10. Thermosphere
11. Mesopause
12. Mesosphere
13. Stratosphere
TROPOSPHERE & WEATHER LAYERS (Sky to Fog)
14. Tropopause — ~5.70–7.60 mi (≈ 30,000–40,000 ft / 9.1–12.2 km) — [Troposphere ceiling]
• Sharp inversion marking the upper boundary of the troposphere.
15. Mid- & upper troposphere — ~1.10–5.70 mi (≈ 6,000–30,000 ft / 1.8–9.1 km) — [Troposphere]
• Dry, fast-moving air; jet streams and frontal systems.
16. Free troposphere [FT] — 0.38–1.10 mi (≈ 2,000–6,000 ft / 0.6–1.8 km) — [Troposphere]
• Subsiding clear air from the North Pacific High, 70s–80s °F.
17. PSI lid [Pacific Subsidence Inversion] — 0.26–0.44 mi (≈ 1,400–2,300 ft / 0.42–0.70 km) — [Troposphere]
• Warm, dry cap sealing humidity beneath; inversion top.
18. Top of marine layer — 0.26–0.44 mi (≈ 1,400–2,300 ft / 0.42–0.70 km) — [Troposphere]
• Upper boundary of fog and onshore circulation, pressed beneath the PSI.
19. Marine layer depth [ML] — 0.19–0.30 mi (≈ 1,000–1,600 ft / 0.30–0.49 km) — [Troposphere]
• Cool, moist fog body connecting ocean, land, and atmosphere.
20. Fog base — 0.08–0.13 mi (≈ 400–700 ft / 0.12–0.21 km) — [Troposphere]
• Lowest visible edge; surface-based cloud deck along coasts and valleys.
21. Fog at ground — 0.00–0.08 mi (≈ 0–400 ft / 0.00–0.12 km) — [Lower Troposphere / Surface Layer]
• Ground-contact fog; the lowest extension of tropospheric cloud,
formed when air temperature equals dew point at the surface—
visibility < ¼ mile (≈ 1,320 ft / 0.40 km), condensation directly at land or sea interface.
Order Summary (Highest → Lowest)
Beyond Observable Universe → Observable Universe Boundary → Cosmic Web →
Interstellar Medium → Heliosphere → Exosphere → Thermosphere → Mesosphere →
Stratosphere → Tropopause → Mid & Upper Troposphere → Free Troposphere [FT] →
PSI Lid → Top of Marine Layer → Marine Layer Depth → Fog Base → Fog at Ground
◯
🜃 nightside magnetotail in the pale,
as radiative cooling resets the inversion.
Enshrouded anew, Alcatraz—the central rock—
in fog-drip hush and advection fog-banks, strata-shifts sway;
upslope fracta-fog climbs the ridgelines,
sky awash in a wind-split drizzly rush—
fleet scud-clouds dash, wisps unravel, radiation mists linger.
The ML spreads its chilling gauze;
fog-cascades spill over ridge-spines,
Ides of fog steered through the Gates of Intros,
condensing to ascend into headlands,
braiding out into extracurricular microclimates.
Sun-holes tear the veil,
inversion-ceiling lid pressed low,
nightlong mistfall beads from a full fog-over—
all adrift within a rose-window span,
thirty miles in radius—
centrifuged Gofcific.
~35°N, 145°W → drifting east world toward the Golden Gate (37.8°N, 122.5°W)
Hadley flow—from the equator northward (ITCZ), pole-star aligned,
gives off the PSI, returning down upon the East Pacific find-out;
where the downward inject stills into layered poise—
descending air beneath the North Pacific High’s realm,
the subsiding zone (Δz ≈ 0.08–0.13 mi thick) taking form aloft,
compresses adiabatically through the six-mile troposphere,
fortifying the PSI’s hold above the sea containing the plush tinct,
settling into coalescence—Arise! above the surface—events to fog.
An empyreal mingling at elevations,
crowned by the cool ML of low blows—
colder air, too dense to rise, halted by that subsiding lid:
a ceiling hanging near 0.40–1.10 mi high.
In early evening beneath summer’s Pacific High,
the ML—marine air mass—compresses down—fog,
yours—ML overhead to the sluice,
ocean energy breaks to sand, giving a hi-hand to invisibilities,
to the rampart shoreline— cosmolatry of opposites—indivisible design.
Down the way, a golden discovery holds—a bright stay of steeped sun;
surface air cooled to the low 60s °F, yet pinned beneath skies
already ~10° warmer above—not cooler!—
coastal landforms cast in real-reel feel,
the ML pulsing down in layered oscillations,
ridges and hills half in cloud,
bridges shifting afore.
Inland to east-splay highs and lows,
the PSI ladders—
lifted by interior heating and pressure gradients,
confining a thinned ML to only a few hundred feet deep,
its base ~0.22 mi (ML base) when eyed from the ground;
fog radiating chilled charges through bare-summer beware,
drifting clouds to sunspots on the QT, foot-out throughput,
brushing the hillsky in greyspraynt, suspended stone-cold—
with surface temps keeping steady in the 60s °F.
Adieu the ML fluxion—of low voes and ria-lands of mid-inland;
the PSI lifts higher,
leaving but a shallow trace of marine grace along the rim;
hills drift, hazed in ocean’s faint refracted light,
at the circlet’s thresholds—where breathings ablend.
The air warms through the upper 70s into the mid-80s,
sealed beneath a steady lid aloft—its grand firmament,
beyond which the free troposphere [FT] thins and dries.
Deeper into the parched interior vales and rolling expanse,
the Marine Layer thins toward vanishing—sun-bleached dustings—
sidewalk air climbing through the 80s and 90s, pushing 100 °F in heatwaves,
while the free troposphere above cools into the 70s near ~1.70 mi
and the 60s by ~2.05 mi; the whole sealed beneath a distant,
diffusing lid, until the inversion loosens its grasp—
threads unspooling—dissolving as the clime climbs
into the dry-up.
Go thy-est again—where transpacific pull renews demand;
step by step through thermolabile gradients along the horizontal,
as the FT grades the vertical.
◯
[Cycle Note]
PSI — low at dawn,
rising high inland by midday,
settling low again at dusk along the coast.
ML — deepest at dawn,
thinning, breaking by noon,
reforming through the evening ride.
◯
KSFO 282353Z 28008KT 5SM PRFG VCFG E SCT020 OVC015 15/14 A3009 RMK HILLS OBSC E
90° along the coastal strip,
NNW inbound winds (from 337.5°, toward 157.5°),
geocoded to shift on Ekman Drive,
shunt surface waters 112.5° along the continental shelf,
colder, nutrient-rich layers rise to fill the void,
cooling the marine boundary layer to near saturation,
a surface-to-air affair—condensate deployed on aerosols,
ocean strata and air converge at rore—
the dew-roar ignition as sea and sky angle into city.
Northwest draws linked valleys into hiding-seeks,
beneath the upper-tropospheric jet, six to eight miles high.
Shaped by this Northern Earth, tilted toward solstice day;
along the edge, the NPH steers the swirl in for the seal,
driving inversion scenes coastward to host the midglide,
sliding beneath the magic foggiest ride,
threading corridors in triplicate intricate,
spilling to film, fill, and frame the QR wind,
venting through fog-belt redwoods ahead—
the inland heat’s switch flicked to [ON]/OFF,
layering frontalities cryptic script again.
◯
≋Air≋ seeded, Forefront Formation Formulae:
into dislocating 🜁⬊╱╲⬋🜂 met,
साँस on chilled cheeks, face-ceptors bare,
startling unmasked AUVs.
Pacific frigorific—surprise.
Enterfog lungs, Oceaterra fog,
into ~112 / 72 mmHg circuits that circumvolve U! in fog-event-the-core—
Flow-of-Gases: (O₂ IN · CO₂ OUT / Air) — ~760 mmHg,
through micropore-secreted gateways.
Bewind among Boatmen,
and ⇡🚲🚶 — designated, combined as [AUVs],
Arise! U Vehicle™ ⚖︎ < 65 lbs —
raised to GPS lines, dropped to wind —
propulse lane ON ≋ destination (un)known.
To parked-OFF, secured, poised,
for another lay of land / ocean sensed.
To return anew—sensorimotor sent,
carried off to another instance,
vitalic formulae: a sensorium send-off.
Foot-Out · Take-Out : Motor-Combiners –
Wheels 🛞 & Bearings ⚙️ : Hub Assembly –
Arise-⇡ Utility-🛹 Vehicle-🏃 : FOTOmachines –
Amplifying the apparent-wind, vehicling through onshore microclimates,
realized in flux and the spired kinetics of fog-gof,
wrought from the inside out, derived from the drive.
A-go, aglow—borne of inspiration,
pressure sets the pulmonary grasp
to sate the gasp: a tableau of Enterfog.
Torque-sensors multiplied, focusing on outdoor gusts,
motor volts call the oxygen draw,
N₂ steadies the breath,
CO₂ tithed to wind,
venting in lung–blood synthesis.
◯
The G.O.F. season is F.O.G.,
Gain-Of-Fog banks.
The California Current—of B.C. Bifurcation—
skirts coastal spires to the 🜁 conveyor,
upwelled coolant—arise!
on the coastal gradient,
advecting shoreward,
wind-inspirited into vantage point,
weaving pyramidal spells
through eddies and gaps,
spilling fast—at Golden Gate rate.
While the crust-illumed
interior’s infrashot 🜁
holds a foothold,
to birrs’ chill—
to
☉
For U, fog-rates stir in the foreground,
the ML stratification deepens...
pooling in hollows...
its crown—the warm cap—pressing...
on the ~0.25-mi-thick, fret-bound layer,
where subsiding air
turns hover-pass into roller-coaster.
As the inland thermal trough sheds its gradients,
winds wend farther inland—slope by tract, block by sock—
advancing through the Central Elements Grid [CEG].
No longer rising,
air parcels settle,
thermal mixing stops,
a stillness takes hold.
Water droplets hang in air,
not falling,
not lifting,
fog fully horizoned,
a deep GOFrific
LOWcific SKYline.
◯
Another setting to ideate the logic of what’s then then,
fog to fog, on a locomotion-mixed journey,
carried by the means of the imaginengine.
ON://INTERLACE→COOL,
sheened with dipalmitoylphosphatidylcholine,
circulation filtered — motion, renewal —
across the span of the Membrane’s Golden Gate.
In quietistic surrealism—scarfed to the 🌞,
an 👁 above clouding clouds, tuned to sea change,
April showers bring May flowers,
modulating through I/O’s brief blooms,
where inspiration opens the astounding stage.
F…
O…
G...
◯
The PSI—Δz ≈ 0.11 mi—dry, subsiding band above an ML ~0.50 mi thick—
caps and couples with an ML in NNW flow, thickened to near 0.50 mi,
suppressing convection, holding the sky beneath its stable frame.
Yet there’s collapse phase—when the layer slims to scarcely 0.06 mi,
it no longer sustains a continuous stratus deck,
but fractures into advected fog-banks and scattered breaks,
raptly sliding low into curtain-walls,
moving pictures a quarter-mile away,
while here stellar colors see in midnight graphic—
apostles to the heliosphere’s aware.
Down lower, condensation energy gathers in latent film,
the city dammed to air in perpetual motion;
and when you step outside, stars stay hidden—
the fog’s already in, its nearness inaugural,
Pacific proximity pressed to the lithosphere.
The sun still shining on and on,
2025 PN₇ in the wondering sky of the moon, the stars and the haze—
cloudflare aimed into peaks, Terres Hautes alight.
Towards the time of machina click,
crystals scrape down from high-sky %;
dawn arises along the mesoscale—
night’s blue ebbing, day’s gold awash.
◯
─────────────────────────────────────
⟦ Form 🜃 ⇄ Flow 🜄 ⇄ Flux 🜁 ⟧
▸ FENCE ID :: SCARFOG® <> BRAND ROSE 🜁T SEA <>
▸ FACE_CLASP :: FAST / SCARF-OPTIONAL-GAITER / FACEMASK – LOWER
▸ PROTOCOL :: (–) FULL-ON-GUARD (+) GAIN-OF-FUNCTION
▸ VIEW-OF-PASSAGE :: IMAGE_FAÇADE_HI-ART
─────────────────────────────────────
⟦ FRAME-OF-GEOAEROGRAPHY ⟧
▸ HORIZON :: TILTED–PACIFIC–CHILLED_54°-EQUINOX-54°
▸ SCUD :: FRONT–OCEAN–GUST_BANK
▸ PANORAMAS :: FLOWSTATE–OF–GRADE
▸ INFRARED :: ATTENUATED_(CERT)
─────────────────────────────────────
⟦ FACILITATION–OF–GAITER ⟧
▸ FERVOR–OF–THE–VEHICLE :: PRESSURED–WEATHERED–VESTURED
▸ VENT–OF–PASSAGE :: FLOW–OF–GRADIENTS
▸ FRONT_IMAGE_OVERLAY :: CUSTOMIQUE–EMBLAZONED
▸ FACEFILM_THERMAL_OFFSET :: FREE–OTHER–GARB
─────────────────────────────────────
⟦ FACING–OPEN–GAUZES ⟧
▸ REAL–TIME_MODULATION :: CAST–ID–YHV 46026 18
▸ MOTIVATOR_SYNC :: FRAME–OF–GO!
▸ FULL–ON–GUARD :: WIND–UVA/UVB–ELEMENTS
▸ OCULUS_SYNC_HOLE(2) :: HISTORIC_SIGNATURE
↳ ΑἰΘΉΡ (UPPER – CELESTIAL AIR)
↳ ἈΉΡ (MIDDLE – MORTAL AIR)
↳ ἈΧΛΎΣ (LOWER – MIST / VEIL / FOG)
─────────────────────────────────────
⟦ FRIGORIFIC–OCTOBERS–GIVEN ⟧
▸ FORWARD_OF_GUARANTEE :: SUN_ANGLES–LOWER_ALEUTIAN–LOW
▸ FORECASTED_OCEANIC–GRADIENT :: SUMMER_SURGE_&_FIRST_PACIFIC–STORMS
▸ SCARFORMULATIONS :: MORE–PLYS–TO–FACE_NPH–RIDGES–AWAY–FROM–COAST
▸ NPH–EQUATORWARD/WEST–SHIFT_PSI–5500BAY-LIFT :: DIABLO WINDS
─────────────────────────────────────
⟦ FORMULATIVE–OBJECTIVE–GAIN/GUIDE ⟧
▸ FABRIC(ATION)–OPTIONS :: GALORE
▸ CONTACT–JUNCTIONS_BUILD :: FOG
▸ FAB–POINTS_INTEGRATION :: GOF
▸ IMPROVISATIONAL–CALCULUS :: FLUX–ORDERED–GRID
▸ ATMOSPHERIC–CATALOG_RELAY :: ACCESSION–SENT
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S I G N A T U R E (–) F O G (+) C A S T ™
