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    • Home (overview)
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  • Cislunar glossary (terms & definitions)

    • Cislunar Space Glossary
    • Dynamics models

      • Circular Restricted Three-Body Problem (CR3BP)
      • CR3BP with Low-Thrust (CR3BP-LT)
      • A2PPO (Attention-Augmented Proximal Policy Optimization)
      • Curriculum Learning
      • Low-Thrust Transfer MDP Formulation
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      • Birkhoff-Gustavson Normal Form
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      • Bicircular Four-Body Problem
      • Quasi-Bicircular Four-Body Problem
      • Strobe Map
      • Stability Set
      • Backward Stability Set
      • Capture Set
      • /en/glossary/dynamics/batch-deployment.html
      • /en/glossary/dynamics/state-dependent-tsp.html
      • /en/glossary/dynamics/q-law.html
      • /en/glossary/dynamics/mass-discontinuity.html
      • /en/glossary/dynamics/equinoctial-elements.html
      • /en/glossary/dynamics/dynamic-programming.html
      • /en/glossary/dynamics/coasting-arc.html
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      • Distant Retrograde Orbit (DRO)
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      • Orbit Identification
      • Transfer Orbit (转移轨道)
      • Perilune (近月点)
      • Apolune (远月点)
      • Retrograde (逆行)
      • Prograde (顺行)
      • Parking Orbit (停泊轨道)
      • Free-Return Trajectory (自由返回轨道)
      • Halo Orbit (Halo 轨道)
      • Lissajous Orbit (Lissajous 轨道)
      • Lyapunov Orbit (Lyapunov 轨道)
      • Cycler Trajectory
      • Multi-Revolution Halo Orbit
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      • /en/glossary/orbits/hub-and-spoke.html
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      • /en/glossary/other/libration-point.html
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      • /en/glossary/other/orbital-residence-platform.html
    • Organizations

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Zonal Wind

Author: CislunarSpace

Site: https://cislunarspace.cn

Definition

Zonal wind is atmospheric horizontal motion blowing along latitude lines (east-west direction). In meteorology: eastward flow is westerly (positive), westward flow is easterly (negative). Zonal wind is a key input parameter for stratospheric airship trajectory planning and energy consumption estimation.

Atmospheric Circulation Framework

Three-cell Circulation Model

Circulation CellLatitude RangeZonal Wind Characteristic
Hadley Cell0-30°NE/SE trade winds (Easterly)
Ferrel Cell30-60°Temperate westerlies
Polar Cell60-90°Polar Easterlies

Seasonal Variation

Typical High-altitude Zonal Wind (@30°N)

Season20 km25 km30 km
Winter-20 m/s-40 m/s-60 m/s
Spring0 m/s-10 m/s-30 m/s
Summer+20 m/s+30 m/s+50 m/s
Autumn0 m/s+10 m/s+20 m/s

Note: Negative = Westerly, Positive = Easterly

Effects on Stratospheric Airships

Trajectory Planning

ImpactDescription
Position driftWind-induced drift rate = vwind×tv_{wind} \times tvwind​×t
Propulsion energyHeadwind navigation requires extra energy
Station-keeping radiusLarger wind speed increases radius maintenance difficulty

Wind Field Modeling

Statistical Model

Based on historical data:

uˉ(h,ϕ,t)=u0(h)+∑i=1NAi(h)cos⁡(ωit+ϕi)\bar{u}(h, \phi, t) = u_0(h) + \sum_{i=1}^{N} A_i(h) \cos(\omega_i t + \phi_i) uˉ(h,ϕ,t)=u0​(h)+i=1∑N​Ai​(h)cos(ωi​t+ϕi​)

Numerical Weather Prediction (NWP)

Modern wind field forecasting uses:

  • WRF (Weather Research and Forecasting)
  • ECMWF Global Model
  • GFS Global Forecast System

Related Concepts

  • Quasi-zero Wind Layer
  • Trajectory Planning
  • Regional Station-keeping Control

References

  • Wallace J M, Hobbs P V. Atmospheric Science: An Introductory Survey[M]. Academic Press, 2023.
  • NOAA. US Standard Atmosphere 1976[M]. US Government Printing Office, 1976.
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Last Updated: 4/29/26, 5:27 PM
Contributors: Cron Job
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