Understanding sounding charts (Skew-T)

For pilots, especially those undertaking long ferry flights over regions like the North Atlantic, understanding weather patterns is critical for safe navigation. The North Atlantic presents some of the most challenging conditions due to its frequent storms, strong winds, and rapidly changing weather. One of the essential tools for pilots to anticipate weather conditions ahead of such flights is the Skew-T log-P chart.

This chart, produced from radiosonde data, offers a comprehensive snapshot of the atmosphere at various altitudes, providing vital information on temperature, humidity, wind, and atmospheric stability. Learning how to interpret these charts gives pilots a detailed picture of what they may encounter, including turbulence, potential storm development, and icing conditions.

In the North Atlantic region, where weather can change quickly and unpredictably, knowing how to read the Skew-T log-P chart helps pilots plan better routes and avoid dangerous weather phenomena, ensuring the safety of both aircraft and crew. It allows them to predict turbulence levels, identify icing layers, and understand wind shear—all of which are crucial for flight planning and making in-flight decisions.

Key Components of the Skew-T Log-P Chart

1. Pressure and Altitude (Y-axis)

The Y-axis represents pressure (in hPa) and altitude (in feet). As you go up the Y-axis, pressure decreases, simulating the ascent of the balloon.

  • The left side shows pressure levels (e.g., 1000 hPa near the surface, 500 hPa around 18,000 ft).

2. Temperature (Skewed X-axis)

The X-axis represents temperature (in °C). The grid lines slant to the right, which is why the chart is called a skew-T. This slant helps visualize the temperature and temperature lapse rates more easily.

  • The red line shows temperature as it changes with altitude.
  • The blue line represents the dew point temperature, which is the temperature at which air becomes saturated and clouds can form.

3. Adiabatic Lapse Rates

  • The green dashed lines represent the dry adiabatic lapse rate (how temperature decreases with altitude when no condensation occurs).
  • The black solid lines represent the moist adiabatic lapse rate (how temperature decreases when the air is saturated).

4. Wind Barbs (Right-hand Side)

On the far right, you see wind barbs, which indicate wind speed and direction at various levels. Each barb points in the direction the wind is coming from. The number of feathers on the barb shows wind speed:

  • Each full feather represents 10 knots, and a half feather represents 5 knots.
  • In your chart, at 16,000 feet, there is a wind from the west (270°) at 34 knots.

5. Key Observations

  • Temperature Profile: The red line shows the temperature profile as you ascend through the atmosphere. In this case, the surface temperature is around 28°C, and as you go higher, the temperature decreases rapidly, reaching -22°C at around 16,000 feet.
  • Dew Point Profile: The blue line represents the dew point, indicating where moisture exists in the atmosphere. The closer the temperature and dew point lines are, the higher the relative humidity and the likelihood of cloud formation. In your image, they are quite far apart, suggesting relatively dry conditions.
  • Wind Speed: The wind speed at 16,000 feet is moderate at 34 knots, with a direction from the west (270°).

Purpose of Skew-T Log-P Charts

These charts are crucial for weather forecasting, allowing forecasters to identify:

  • Atmospheric stability (e.g., potential for thunderstorms or clear weather),
  • Moisture content (cloud formation),
  • Wind patterns at different altitudes.

The chart helps determine instability, which is key for predicting severe weather. If the temperature decreases more rapidly with height than the adiabatic lapse rates suggest, the atmosphere is unstable, potentially leading to thunderstorms.

Final Thoughts

Understanding the Skew-T log-P chart provides pilots with a reliable tool to predict weather conditions, particularly when flying over challenging areas like the North Atlantic. Mastering its interpretation can significantly enhance flight safety, enabling pilots to make informed decisions and navigate safely through turbulent or unstable weather systems.