Wind Effects on the Launch Loop

Wind, hail, ice accumulation and lightning are hazards for launch loops, deflecting or damaging the incline track. A launch loop should be able to survive 20 year and perhaps 50 year extremes in these conditions. The launch loop will be built over the equatorial ocean, far from large populations, in case of failure. So our concern is the weather over the best sites in the equatorial ocean.

Predictable, slowly changing winds can be accommodated by changing the deflection angles at the ground. Unpredictable gusty winds will add forces that can lead to instability and failure. How much wind can we accommodate?

Assume that the peak wind is 39 knots, about 20 meters per second. The cross section of the launch loop through the atmosphere is about 0.1 meters, with a drag coefficient of about 1. It traverses the troposphere and lower stratosphere (up to an estimated 20km) at an angle of about 19 degrees, thus exposing about 60km of forward and reverse track to the wind, an area of 12000m² . The higher altitude air is less dense, but may be moving faster. The drag is the density (1.2kg/m³) times the velocity squared times the drag coefficient and area - 480 Pa * 12000 m² = 5.8E6 Newtons, which deflects the tracks by about 0.01 radians or about 0.6 degrees. While that seems small, if uncorrected that is enough to miss the stations by 3 kilometers. Since the spacing accommodation of the track and station magnets is on the order of 5 millimeters, we would need to be able to measure and predict the average wind along the track with an error less than 1 part per million over the 20 seconds between the time the rotor leaves the station and the time it passes through the troposphere.

We can deal with unpredictable gusty winds in seven ways, in order of cost:

• 1) locate the launch loop in areas with very low wind shear 2) get extremely good at wind measurement and prediction over the next 30 seconds 3) add moving counterweights near the track 4) add actively adjusted tensioning cables to the ground 5) add propulsion devices along the track (propellers, shutters) 6) scale up the mass-to-area ratio 7) accept a higher failure rate

It is not wind that causes the problem, it is variable winds, which are caused by wind shear and turbulence. Where two air masses move past each other at different speeds or in different directions there will be wind shear, which causes rotating vortexes near the boundary. Where high moisture hot air rises through low moisture air, the air column is unstable, and there will be up and down drafts. The air mostly heats via the ocean surface, so shading by scattered clouds creates cooler and warmer patches. All these effects make the air chaotic and hard to predict.

  Big whorls have little whorls
   That feed on their velocity,
 And little whorls have lesser whorls
   And so on to viscosity.

  -- Lewis F. Richardson, pioneer of numerical weather prediction

The map below shows the tracks of hurricanes for the last century, and the range of the Inter Tropic Convergence Zone, from the southern line in January to the northern line in July. The zone is where westerly trade winds from the southern and northern hemispheres merge and rise, driven by hot moist air from the summer ocean. Hurricanes generally start in the tropics, north of 5 degrees north latitude, or south of 5 degrees south latitude.