This prediction market asks whether Wellington's highest temperature will be exactly 12°C on May 2, 2026. Wellington in early May is autumn in New Zealand, with typical daily highs ranging from 11–15°C depending on prevailing weather patterns and frontal systems. The 0% current odds reflect a fundamental mathematical reality: actual temperatures are continuous measurements, so hitting exactly 12.0°C is extraordinarily unlikely. Weather prediction markets typically see such precision-dependent outcomes receive minimal trading interest because the inherent probability is so small. Traders who have assessed this market recognize that even a forecast high of 12.0°C has virtually zero chance of measuring exactly that value—it could be 11.8°C, 12.1°C, 12.3°C, or any other nearby value. The low trading volume ($1,157 in 24h) further reflects rational skepticism about the resolution criteria and the specificity of the question. For this market to resolve YES, official Wellington weather data must record the maximum temperature as exactly 12°C, measured according to whatever standard the resolution source applies.
Deep dive — what moves this market
Wellington's climate in May is transitional autumn, shaped by its position on New Zealand's North Island at latitude 41°S. The city experiences cool, variable conditions as southern polar air masses interact with subtropical moisture, creating conditions that rarely stabilize into a single predictable pattern. Daily maximum temperatures in early May typically range from 10–16°C, with significant day-to-day variability. The question posed—whether the highest temperature on a specific day will be exactly 12°C—represents an extreme precision requirement that goes against how modern meteorological measurement works. Temperature readings are taken continuously and reported to decimal precision (12.1°C, 12.3°C, 11.8°C), not in whole-degree increments. For a day's maximum to resolve as exactly 12°C, either the measurement must genuinely peak at that value, or the resolution mechanism must apply rounding rules that happen to round the true maximum to 12°C. Weather patterns pushing Wellington toward warmer maxima would include anticyclonic systems bringing warm northerly flows, or föhn winds across Cook Strait that warm air adiabatically. Conversely, cold southerly outflows or frontal rain bands would suppress temperatures. A typical cool autumn high in the 10–12°C range would require settled conditions with limited solar heating—possible but not guaranteed. A high exactly at 12°C would require the daily peak to fall within an extremely narrow window, competing against dozens of other possible values. Traders pricing this at 0% odds are making a rational assessment: the chance that May 2 in Wellington peaks at exactly 12.0°C (and resolves as such) is negligible. Even if meteorologists forecast a high near 12°C, actual temperatures drift based on cloud cover timing, wind speed, and microclimatic factors. The resolution source (likely New Zealand's MetService) will report a temperature, but the probability of that being exactly 12 rather than 11, 13, or 12.1 is mathematically tiny. This market exemplifies why highly specific numeric outcomes in weather prediction markets attract almost no volume and virtually no YES traders. The question is technically resolvable, but the prior probability is so low that rational traders see no value in taking either side.