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The Nicaragua Winds: Enhanced Trades and Papagayo

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The Nicaragua Winds: Enhanced Trades and Papagayo

The Wind in Nicaragua: Enhanced Trade Winds

The wind conditions in the lake district of Nicaragua are generally attributable to an enhanced trade wind effect. At the earth's heat equator, air rises creating an area of low pressure called the Inter Tropical Convergence Zone or ITCZ for short. The air rises up to the tropopause before diverging poleward. At approximately 30 degrees of latitude, this poleward flow meets a descending air-mass and is forced back down to earth creating a belt of high pressure. A surface pressure gradient is setup between the two areas, with the high pressure area being approximately 30 degrees from the equator and the low pressure being roughly at the equator. Nature attempts to equalize the pressure gradient with a resultant surface flow of air know as a 'Trade Wind'. In Central America the Trade Winds cannot flow freely because of the Central American Cordillera Mountain range, which creates a physical barrier between the Subtropical high pressure and equatorial low pressure. The only points of release for the build of pressure is at breaks in the Cordillera mountain range, the most significant one of which is the valley formed by Lake Nicaragua. As such, the low lying lake district of Nicaragua can be likened to a pressure release valve - with an entire regions worth of airflow being funneled through it. During the Northern hemisphere winter, when the ITCZ is further South and the Trade Wind's are stronger, the resultant flow of air whistles across the lake at a steady 17kts to 25kts.

The Wind in Nicaragua: Papagayo Events

As described above, the Nicaragua lake district can be likened to the 'pressure relief valve' for the Central American Isthmus - one of few points at which air can flow unimpeded from the subtropical high to the equatorial low. Now imagine the scenario in the US fall, winter & spring when a mammoth sized, frozen, super-dense, high pressure air mass drifts South off the Great Plains to the Gulf of Mexico and the Caribbean. Its like a car tire being pumped up... and up... and up... until the high pressure eventually reaches the gap in the Cordillera at Lake Nicaragua... when the valve rips off and the air rushes out explosively. At this point you have the entire force of the Great Plains winter freeze combining with the already strong subtropical high being squeezed through a 99 mile wide funnel creating a massive scale venturi. The resultant 'Papagayo Winds' shriek across the lake at speeds normally seen only in major hurricanes - but the weather is warm & the skies are clear. Though a spectacle to behold, the force of nature witnessed during a 'Papagayo Event' is simply too much for kitesurfing in the Rivas area. During Papagayo Events the spots at the extreme northern & southern ends of the lake remain manageable with steady wind speeds in the 30kt to 40kt range.