⟿ CRYDON MESOSCALE METEOROLOGY · CAIRNGORM SUMMIT · EST. MMXXIV ⟿

The Atmosphere
is a sculpture

Crydon does not forecast weather. We read the air. In the pressure gradients that bend the wind, in the CAPE values that birth thunderstorms, in the isobars that map the invisible—we find the architecture of the sky. The atmosphere is not chaos. It is a language. We are learning to speak it.

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⟿ CRYDON · MESOSCALE METEOROLOGY · EST. MMXXIV · STATION 54°N 2°W ⟿
⟿ Atmospheric Parameters · Live Feed ⟿
The Variables
► CONVECTIVE AVAILABLE POTENTIAL ENERGY
CAPE
2450 J/kg · MODERATE SEVERE

The Fuel

The energy available for convection—the atmospheric gasoline. When CAPE exceeds 2000 J/kg, the atmosphere is primed for explosive development. Updrafts can punch through the troposphere at 60 m/s, carrying moisture into the stratosphere. We track CAPE not as a number but as a threshold. Beyond it, the sky rewrites itself.

► JET STREAM
Wind Shear
45 KT · 250 MB · SW→NE

The Sculptor

At 30,000 feet, the jet stream carves the atmosphere like a riverbed. Wind shear—the change in speed and direction with height—determines whether a storm rotates or collapses. 45 knots of deep-layer shear is the sweet spot: enough to tilt the updraft, vent the top, let the storm breathe. Too much, and the storm tears itself apart. We measure the difference in meters per second.

► PRESSURE GRADIENT
Isobar
4 HPA/100KM · TIGHTENING

The Force

Pressure gradient is the atmosphere's gravity—the force that moves everything. Four hectopascals per hundred kilometers means the wind will howl. The tighter the isobars, the steeper the slope the air must climb. We watch the gradient tighten on our screens and know: the atmosphere is about to move. Not tomorrow. Now.

⟿ CAIRNGORM SUMMIT · 54°N 2°W · ELEV 1245M ⟿
⟿ Station Telemetry ⟿
The Readings
1245M
◯ ELEVATION
-6.2
◯ LIFTED INDEX
45KT
◯ WIND SHEAR
∞
◯ ATMOSPHERIC DEPTH
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The Summit

⟿ Crydon Station ⟿

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Crydon Met Station
Cairngorm Mountain, Aviemore PH22 1RB, UK
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