Trader sentiment for the August 27 rainfall market is now driven by post-event verification against National Weather Service and NOAA precipitation data rather than forecasts. Official gauge measurements, radar estimates, and quality-controlled totals from that date determine resolution, with any model-observation mismatches potentially shifting final outcomes. Late-August climatology typically features scattered convective showers tied to diurnal heating and weak fronts, yet the actual geographic pattern hinged on that day's specific moisture transport and instability. No additional data releases remain pending as the period has concluded, enabling direct comparison of historical analogs to the measured distribution.
Résumé expérimental généré par IA à partir des données Polymarket. Ceci n'est pas un conseil de trading et ne joue aucun rôle dans la résolution de ce marché. · Mis à jourOù va-t-il pleuvoir le 27 août ?
$6,272 Vol.
New York, NY
Oui
Los Angeles, CA
Non
Chicago, IL
Non
Houston, TX
Non
Dallas, TX
Non
Phoenix, AZ
Non
Philadelphie, PA
Oui
Denver, CO
Non
Washington, DC
Oui
Atlanta, GA
Oui
Miami, FL
Oui
Seattle, WA
Non
Boston, MA
Non
La Nouvelle-Orléans, LA
Oui
San Francisco, CA
Non
$6,272 Vol.
New York, NY
Oui
Los Angeles, CA
Non
Chicago, IL
Non
Houston, TX
Non
Dallas, TX
Non
Phoenix, AZ
Non
Philadelphie, PA
Oui
Denver, CO
Non
Washington, DC
Oui
Atlanta, GA
Oui
Miami, FL
Oui
Seattle, WA
Non
Boston, MA
Non
La Nouvelle-Orléans, LA
Oui
San Francisco, CA
Non
Measurable precipitation means 0.01 inches or more as reported by the PRECIPITATION (IN) figure in the NWS Daily Climate Report (CLI) for the city's station.
A report of trace ("T") does not qualify.
The PRECIPITATION (IN) figure measures total liquid-equivalent precipitation and does not distinguish between precipitation types.
The observation period is the NWS climate day for KNYC: midnight to midnight local standard time. The final CLI report for a climate day is issued the following morning.
Resolution is based on the most recent CLI report published for the observation date. If multiple versions of the report are issued, the last version published before 11:59 PM ET on the day following the observation date governs. If no figure has been published by that time, this market will resolve to "No".
The resolution source for this market is the NWS Daily Climate Report (CLI) for KNYC, published at https://forecast.weather.gov/product.php?site=NWS&product=CLI&issuedby=NYC.
Marché ouvert : Aug 27, 2026, 7:09 AM ET
Source de résolution
https://forecast.weather.gov/product.php?site=NWS&product=CLI&issuedby=NYCRésolveur
0x65070BE91...Résultat proposé: Oui
Contesté
Résultat proposé: Oui
Contesté
Résultat final: Oui
Measurable precipitation means 0.01 inches or more as reported by the PRECIPITATION (IN) figure in the NWS Daily Climate Report (CLI) for the city's station.
A report of trace ("T") does not qualify.
The PRECIPITATION (IN) figure measures total liquid-equivalent precipitation and does not distinguish between precipitation types.
The observation period is the NWS climate day for KNYC: midnight to midnight local standard time. The final CLI report for a climate day is issued the following morning.
Resolution is based on the most recent CLI report published for the observation date. If multiple versions of the report are issued, the last version published before 11:59 PM ET on the day following the observation date governs. If no figure has been published by that time, this market will resolve to "No".
The resolution source for this market is the NWS Daily Climate Report (CLI) for KNYC, published at https://forecast.weather.gov/product.php?site=NWS&product=CLI&issuedby=NYC.
Source de résolution
https://forecast.weather.gov/product.php?site=NWS&product=CLI&issuedby=NYCRésolveur
0x65070BE91...Résultat proposé: Oui
Contesté
Résultat proposé: Oui
Contesté
Résultat final: Oui
Trader sentiment for the August 27 rainfall market is now driven by post-event verification against National Weather Service and NOAA precipitation data rather than forecasts. Official gauge measurements, radar estimates, and quality-controlled totals from that date determine resolution, with any model-observation mismatches potentially shifting final outcomes. Late-August climatology typically features scattered convective showers tied to diurnal heating and weak fronts, yet the actual geographic pattern hinged on that day's specific moisture transport and instability. No additional data releases remain pending as the period has concluded, enabling direct comparison of historical analogs to the measured distribution.
Résumé expérimental généré par IA à partir des données Polymarket. Ceci n'est pas un conseil de trading et ne joue aucun rôle dans la résolution de ce marché. · Mis à jour
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