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Rossby wave breaking (RWB) Definition Detection / Measurement Climatology Dynamics – Impact on internal variability (NAO / NAM) – Impact on surface turbulent heat flux (PDO)
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Definition 350 K Potential Vorticity, 1-8 July 1998 - Wave amplitude reaches critical level - Irreversible overturning of isentropic potential vorticity PVU Data: NCEP / NCAR Reanalysis
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PVU Anticyclonic RWB Cyclonic RWB Detection / measurement Centroid of low-P lobe
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Climatology: DJF 1958-2006 Antic Cycl contours are relative frequency shading is zonal extent
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Climatology 1958-2008 Relative frequency:
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Rossby wave breaking (RWB) Definition Detection / measurement Climatology Dynamics – Impact on internal variability (NAO / NAM) – Impact on surface turbulent heat flux (PDO)
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Dynamics Impact on internal variability (NAO / NAM) – Forces the background flow via, primarily, eddy momentum flux convergence – Generates surface pressure anomalies Impact on surface turbulent heat flux (PDO) – Generates coherent, 3D circulations associated with temperature and moisture anomalies
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Forcing of background flow Look at composite divergence of E fields around hundreds of RWB centroids Hoskins et al. (1983)
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SLP
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Regions where RWB forces NAO Pos. Neg.
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Dynamics Impact on internal variability (NAO / NAM) – Forces the background flow via, primarily, eddy momentum flux convergence – Generates surface pressure anomalies Impact on surface turbulent heat flux (PDO) – Generates coherent, 3D circulations associated with temperature and moisture anomalies
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Pacific Decadal Oscillation Leading pattern of extratropical Pacific sea surface temperature variability Data: NOAA ESRL SST V2 “warm” “cool”
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Pacific Decadal Oscillation Alexander et al. (2002) Journal of Climate Anticyclonic and cyclonic RWB
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D D Negative indicates into the ocean Anticyclonic RWB Composite of 200 randomly Selected winter cases
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U U Negative indicates into the ocean Cyclonic RWB Composite of 200 randomly selected winter cases
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RWB Variability (EOFs) Relative frequency: All four patterns are significantly correlated with the current and future PDO (e.g., January)
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Effect of Cyclonic Dec-Jan RWB
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200 randomly selected cases
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Effect of Cyclonic Dec-Jan RWB 200 randomly selected cases
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Effect of Anticyclonic Jul-Aug RWB 200 randomly selected cases
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RWB Variability (EOFs) Relative frequency: All four patterns are significantly correlated with the current and future PDO (e.g., January)
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Statistical Model of PDO using RWB Cross validation Stepwise bootstrapping Model any month
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Rossby wave breaking (RWB) Definition Detection / Measurement Climatology Dynamics – Impact on internal variability (NAO / NAM) – Impact on surface turbulent heat flux (PDO)
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Rossby wave breaking PVU 350 K, July 1998, NCEP / NCAR Reanalysis data - Wave amplitude reaches critical level - Irreversible overturning of isentropic potential vorticity PVU
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Cyclonic Rossby wave breaking PVU Potential vorticity on the 350-K surface, January 2003 PVU
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