(Noh et al., 2026)
RHYB is a Regional hybrid blocking detection method that requires both an amplitude criterion on the geopotential height anomaly and a flow reversal criterion. Rather than applying a single amplitude threshold across the Northern Hemisphere, it sets the threshold from the local geopotential height variability at each grid point and for each month, so that blocking is detected consistently even over the low-variability Eurasian interior and in summer.
This design follows Noh et al. (2026); the data provided here extend it with a monthly adjustment so that the method can be applied in all seasons.
Noh, H., Ku, HY., Sung, MK. et al. Uncovering missing Eurasian blocking events and their robust role in East Asian winter extremes: a region-dependent detection approach. npj Clim Atmos Sci 9, 144 (2026). https://doi.org/10.1038/s41612-026-01415-7
Blocking frequency is updated daily from NOAA CORe daily-mean 500-hPa geopotential height (Z500), with a lag of a 2 days. Occasional data delays are usually resolved within a few days. Blocking is detected with the Regional Hybrid (RHYB) method.
Panel (a) shows the climatological number of blocked days for the month (1979 to the previous year). Panel (b) shows the number of blocked days in the current month to date (days 1–N). Panel (c) shows the anomaly: (b) minus the climatology for the same N days. Units are days.
The map shows the most recent day available. Shading indicates the Z500 anomaly (gpm) relative to the 1979–2025 climatology for the same calendar day. Black contours show Z500 at 60-gpm intervals. Green contours outline blocking detected by RHYB.