Fig. 7: Lag correlation of \({P}_{{10}^{\circ }{{S}}-{10}^{\circ }{{N}}}^{20-100{\rm{day}}}\) at all longitudes with \({P}_{{10}^{\circ}{{S}}-{10}^{\circ}{{N}}}^{20-100{\rm{day}}}\) averaged from 80 °E to 100 °E (ref. 42). | npj Climate and Atmospheric Science

Fig. 7: Lag correlation of \({P}_{{10}^{\circ }{{S}}-{10}^{\circ }{{N}}}^{20-100{\rm{day}}}\) at all longitudes with \({P}_{{10}^{\circ}{{S}}-{10}^{\circ}{{N}}}^{20-100{\rm{day}}}\) averaged from 80 °E to 100 °E (ref. 42).

From: ACE2: accurately learning subseasonal to decadal atmospheric variability and forced responses

Fig. 7

\({P}_{1{0}^{\,{\circ }}{{S}}-1{0}^{\,{\circ }}{{N}}}^{20-100{\rm{day}}}\) is the surface precipitation rate averaged from 10 °S to 10 °N, and then filtered with a 20–100 day bandpass filter. Calculated over the 2001–2010 period from a ERA5, b the test period run of ACE2-ERA5 and c the first ensemble member of the SHiELD AMIP run.

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