Linked from

The 32 pages that link to Hadley cell, each with the reason it gives.

• Rain shadowRelated: Its descending dry air creates broad arid belts without requiring mountain barriers.

• ConvectionBroader topic: It shows how solar heating drives large-scale atmospheric convection and circulation.

• Mediterranean climateNarrower topic: Its descending branch helps create the high-pressure belts behind summer dryness.

• Atmospheric circulationBroader topic: It carries heat from the tropics toward subtropical latitudes.

• Trade windsBroader topic: The circulation now bearing Hadley’s name supplies the modern framework for explaining the trades.

• Intertropical Convergence ZoneRelated: The convergence zone marks the rising branch of this circulation.

• ClimateBroader topic: Its rising and sinking branches help organize tropical rainfall and subtropical deserts.

• Tropical climateRelated: Its rising branch supports tropical rainfall, while its sinking branch shapes nearby dry zones.

• Arid climateRelated: Its descending dry air helps create major belts of subtropical aridity.

• Jet streamRelated: Its poleward upper-level flow contributes to the subtropical jet.

• WesterliesNarrower topic: Its descending branch helps set the subtropical boundary of the westerly wind belt.

• Desert climateRelated: Its descending, drying air helps form many subtropical deserts.

• East Asian monsoonNarrower topic: Its seasonal shifts help shape subtropical pressure belts bordering East Asia.

• Subtropical ridgeRelated: The descending branch of this circulation helps sustain the ridge.

• Walker circulationRelated: It is the north–south circulation that operates alongside the Walker circulation’s east–west loop.

• Atmosphere of MarsRelated: Mars’s seasonal heating drives broad circulation that transports heat and dust across the planet.

• Tropical savanna climateNarrower topic: Its rising and sinking branches underpin the seasonal circulation that shapes rainfall.

• TroposphereRelated: It is a large-scale circulation pattern operating within the troposphere.

• AnticycloneNarrower topic: Descending branches help establish the subtropical high-pressure belts where anticyclones often form.

• Tropical rainforest climateRelated: Its rising equatorial branch supplies the broad circulation behind persistent tropical convection.

• Humid subtropical climateRelated: Its shifting circulation helps steer subtropical high-pressure systems and seasonal rain belts.

• Semi-arid climateNarrower topic: Descending subtropical air suppresses rainfall across many semi-arid regions.

• Australian monsoonNarrower topic: The monsoon operates within the larger seasonal circulation linking tropical ascent and subtropical subsidence.

• AridificationRelated: Shifts in its descending dry-air belt can alter subtropical rainfall.

• Atmosphere of VenusRelated: It helps transport heat through Venus’s deep atmosphere.

• Dry seasonRelated: Descending branches suppress clouds and rainfall in many dry-season regions.

• Wet seasonNarrower topic: Its shifting rain and descent belts help explain broad seasonal rainfall patterns.

• Desert (geography)Related: Descending dry air helps form many of the world's subtropical deserts.

• NamibNarrower topic: Descending subtropical air contributes to the region’s persistent aridity.

• Prevailing windsBroader topic: Its surface return flow produces the trade winds.

• SubtropicsRelated: Its descending air creates many of the subtropics’ dry, stable conditions.

• Zonal and meridional flowBroader topic: Its north–south overturning is a large-scale meridional circulation.