S&P 500 vs. Ap Index (May–Nov 2026). Projected Ap Index Peaks (+4-Day Lag) = Expected S&P 500 Lows:
Oct 14 (Wed), Oct 17 (Sat), Oct 26 (Mon), Nov 4 (Wed), Nov 13 (Fri), Nov 22 (Sun).
The time it takes for a Coronal Mass Ejection (CME) to reach the Earth depends on several factors, such as the speed of the CME, the density of the solar wind, and the position of the Earth relative to the Sun. On average, a CME can take anywhere from 1 to 5 days to reach the Earth: fast CMEs (speeds > 1000 km/s) 1-2 days, average CMEs (speeds ~500-1000 km/s) 2-3 days, and slow CMEs (speeds < 500 km/s) 3-5 days.
Geomagnetic disturbances (elevated Ap index) are hypothesized to subtly impair collective mood and heighten risk aversion. Market participants may misattribute this psychological distress to economic fundamentals, leading elevated Ap to precede S&P 500 lows and trend reversals by a short lag of a few calendar days.
To evaluate this relationship, historical NOAA 45-day Ap forecasts (updated daily) were parsed into a continuous daily series using the most recent available issues. These values were correlated against daily S&P 500 close-to-close and absolute returns across 0 to +5 calendar-day lags from January 1, 2020, to present. Across the full sample, the 45-day forecast displays only modest directional correlation with next-day price movements; its primary statistical signal is a positive link to subsequent absolute returns (volatility), currently peaking around +4 to +5 days.
However, this optimal lag lacks long-term stability—holding near +4 days throughout the summer and early fall before shifting in recent windows—reflecting the limited predictive skill of multi-week geomagnetic forecasts. Comparative analysis shows that NOAA's 27-day Ap outlook provides neither stronger directional lead times nor greater stability than the 45-day series. Because the 27-day projection updates only weekly, its lower publication frequency introduces additional noise, making lead-lag relationships harder to measure than in the daily 45-day series.
The Ap Index (used in NOAA's 45- and 27-day forecasts) is the linear counterpart of the quasi-logarithmic Kp Index (used in NOAA's 3-day forecast). Each 3-hour Kp value converts to an equivalent amplitude via a fixed table (Kp 0→0, 1→3, 2→7, 3→15, 4→27, 5→48, 6→80, 7→140, 8→240, 9→400); the daily Ap is the average of those eight 3-hour values. The two indices therefore track the same geomagnetic activity on different scales.
To evaluate this relationship, historical NOAA 45-day Ap forecasts (updated daily) were parsed into a continuous daily series using the most recent available issues. These values were correlated against daily S&P 500 close-to-close and absolute returns across 0 to +5 calendar-day lags from January 1, 2020, to present. Across the full sample, the 45-day forecast displays only modest directional correlation with next-day price movements; its primary statistical signal is a positive link to subsequent absolute returns (volatility), currently peaking around +4 to +5 days.
However, this optimal lag lacks long-term stability—holding near +4 days throughout the summer and early fall before shifting in recent windows—reflecting the limited predictive skill of multi-week geomagnetic forecasts. Comparative analysis shows that NOAA's 27-day Ap outlook provides neither stronger directional lead times nor greater stability than the 45-day series. Because the 27-day projection updates only weekly, its lower publication frequency introduces additional noise, making lead-lag relationships harder to measure than in the daily 45-day series.
The Ap Index (used in NOAA's 45- and 27-day forecasts) is the linear counterpart of the quasi-logarithmic Kp Index (used in NOAA's 3-day forecast). Each 3-hour Kp value converts to an equivalent amplitude via a fixed table (Kp 0→0, 1→3, 2→7, 3→15, 4→27, 5→48, 6→80, 7→140, 8→240, 9→400); the daily Ap is the average of those eight 3-hour values. The two indices therefore track the same geomagnetic activity on different scales.
NOAA's latest 3-day forecast above shows a peak Kp of 5 (equivalent Ap ≈ 48) on Tuesday, October 13, between 06:00 and 09:00 UTC (2:00–5:00 a.m. ET). Shifting that interval forward by three calendar days points to Friday, October 16; a four-day shift points to Saturday. This suggests another S&P 500 low may arrive by the end of the trading week.
To evaluate shorter-term dynamics, 180 days of NOAA 3-day Kp forecasts were compiled, converted to 3-hour equivalent Ap, adjusted to Eastern Time (ET), and exhaustively tested across lags of 0 to 120 hours against hourly S&P 500 closes to identify the shift with the strongest negative correlation to price level. The latest weekly charts above display hourly S&P 500 OHLC bars (left scale) overlaid with the 3-hour equivalent Ap series shifted forward by the optimal +45 hours on an inverted right scale. Each panel spans Saturday through the following Sunday to show the complete trading week in context.
This optimal +45-hour lag differs from the +3 to +5 calendar-day lag observed on daily Ap charts because the NOAA 3-day forecast model (updated twice daily at 00:30 and 12:30 UTC; during EDT / UTC−4, this corresponds to 8:30 p.m. ET the previous day and 8:30 a.m. ET the same day) evaluates high-resolution, short-horizon Kp/Ap data against hourly prices over a shorter sample window, where forecast decay and short-term noise shift the best-fit alignment relative to multi-month realized daily Ap metrics.
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