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Figure 4c Cross correlation statistics of the average lag between the peak monthly rates of change of the global average 700 mb specific humidity (NCEP Reanalysis) versus the global average lower tropospheric air temperature (Figure 4b) anomaly (RSS TLT) over the base perioc of 1980 - 2016.

Figure 4 c Cross correlation statistics of the average lag between the peak monthly rates of change of the global average 700 mb specific humidity (NCEP Reanalysis) versus the global average lower tropospheric air temperature (Figure 4b) anomaly (RSS TLT) over the base perioc of 1980 - 2016.

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1970 1972 1974 1976 1978 1980 1982 1984 1986 1988 1990 1992 1994 1996 1998 2000 2002 2004 2006 2008 2010 2012 2014 2016 2018
Figures 2a and 2b Comparisons of the seasonally detrended (12 month average) anomalies of the tropical Pacific Trade Wind Speed (240W — 90W x 5N — 5S, 850 mb) versus the global average tropical sea surface temperature (360W — OW x 5N — 5S) and their associated monthly derivatives, respectively, from NCEP Reanalysis.
Figures 2a and 2b Comparisons of the seasonally detrended (12 month average) anomalies of the tropical Pacific Trade Wind Speed (240W — 90W x 5N — 5S, 850 mb) versus the global average tropical sea surface temperature (360W — OW x 5N — 5S) and their associated monthly derivatives, respectively, from NCEP Reanalysis.
Figure 2c Cross correlation statistics of the average lag between the peak monthly rates of change of the global tropical sea surface temperature versus the Pacific Trade Wind Speed (Figure 2b) over the base period of 1980 - 2016.
Figure 2c Cross correlation statistics of the average lag between the peak monthly rates of change of the global tropical sea surface temperature versus the Pacific Trade Wind Speed (Figure 2b) over the base period of 1980 - 2016.
Figures 3a and 3b The seasonally detrended (12 month average) global average specific humidity (360W — OW x 90N — 90S, 700 mb) and the comparison of the monthly rates of change of the of the global average specific humidity and the global average tropical sea surface temperature, respectively, from NCEP Reanalysis.
Figures 3a and 3b The seasonally detrended (12 month average) global average specific humidity (360W — OW x 90N — 90S, 700 mb) and the comparison of the monthly rates of change of the of the global average specific humidity and the global average tropical sea surface temperature, respectively, from NCEP Reanalysis.
Figure 3c Cross correlation statistics of the average lag between the peak monthly rates of change of the global tropical sea surface temperature versus the 700 mb global average specific humidity (Figure 3b) over the base period of 1980 - 2016.
Figure 3c Cross correlation statistics of the average lag between the peak monthly rates of change of the global tropical sea surface temperature versus the 700 mb global average specific humidity (Figure 3b) over the base period of 1980 - 2016.
Figures 4a and 4b The seasonally detrended (12 month average) anomaly of the global average lower tropospheric air temperature (RSS TLT) and the comparison of its associated monthly rate of change versus the 700 mb global average specific humidity (NCEP Reanalysis), respectively.
Figures 4a and 4b The seasonally detrended (12 month average) anomaly of the global average lower tropospheric air temperature (RSS TLT) and the comparison of its associated monthly rate of change versus the 700 mb global average specific humidity (NCEP Reanalysis), respectively.
Figure 6c Cross correlation statistics of the average lag between the peak monthly rates of change of the Pacific Trade Wind Speed (NCEP Reanalysis) versus the global average atmospheric angular momentum (Figure 5b) anomaly (NOAA ESRL) over the base period of 1980 - 2014.
Figure 6c Cross correlation statistics of the average lag between the peak monthly rates of change of the Pacific Trade Wind Speed (NCEP Reanalysis) versus the global average atmospheric angular momentum (Figure 5b) anomaly (NOAA ESRL) over the base period of 1980 - 2014.
Average Lag (Tau) in Months After the Easterly Pacific Trade Winds Attain their Peak Deceleration
Average Lag (Tau) in Months After the Easterly Pacific Trade Winds Attain their Peak Deceleration
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