Hammy wrote:Is there any way to check this in real time as a potential factor this year?
I don't know of any real time way to check the current strength of the thermohaline circulation, though I imagine daily data for the variables used in Klotzbach and Gray's formulation of their THC proxy.
Reading through their
2013 verification report, there's a section that discusses their THC proxy. If I'm reading it right, their formula is the standard deviation of the surface meridional wind anomaly plus the standard deviation of the SST anomaly minus the standard deviation of the sea-level pressure anomaly (all concerning the Eastern Atlantic).
Using the NCEP Reanalysis Dataset over at ESRL I decided to use their formula to see what their THC proxy would say for this year. According to my calculations the THC proxy increased significantly between March and May 2017, and is presently quite positive. However, my calculations might be wrong because my values for 2013 don't match their published 2013 THC values (though that may be due to different datasets used; however, the general trends are somewhat there).
Regardless of the raw values, the qualitative parameters for a strong THC according to Klotzbach/Gray's formulation are all there. May 2017's Eastern Atlantic meridional wind anomalies were anomolously southerly (and, in fact, the most southerly for any May since the NCEP dataset began in 1948). Sea surface temperature anomalies were also anomolously warm, and the second warmest of any May since 1948 (behind 1995). May 2017's Eastern Atlantic sea level pressure anomalies were also anomolously low, and were the lowest May pressures for the region since records began in 1948.