The Bottom panels (C and D) show the unconditional probability (across the ensemble) that
the annual precipitation anomaly is less than — 0.5 SDs, and the conditional probability that both
the annual precipitation anomaly is less than — 0.5 SDs and the temperature anomaly is greater than 0.
Bottom row:
Annual precipitation anomaly for 2017 relative to the annual average for the period 1981 - 2010.
Annual precipitation anomalies vary about zero, with relatively dry periods centered on 0.5 and 1.4 ka.»
Not exact matches
southern oscillation a large - scale atmospheric and hydrospheric fluctuation centered in the equatorial Pacific Ocean; exhibits a nearly
annual pressure
anomaly, alternatively high over the Indian Ocean and high over the South Pacific; its period is slightly variable, averaging 2.33 years; the variation in pressure is accompanied by variations in wind strengths, ocean currents, sea - surface temperatures, and
precipitation in the surrounding areas
Anomalies in
annual average
precipitation in mm per day in three experiments: (a) wNA, (b) Amazon, (c) wNA + Amazon.
Top row:
Annual European precipitation anomalies from 1979 to 2017, relative to the annual average for the period 1981 -
Annual European
precipitation anomalies from 1979 to 2017, relative to the
annual average for the period 1981 -
annual average for the period 1981 - 2010.
Global solar irradiance reconstruction [48 — 50] and ice - core based sulfate (SO4) influx in the Northern Hemisphere [51] from volcanic activity (a); mean
annual temperature (MAT) reconstructions for the Northern Hemisphere [52], North America [29], and the American Southwest * expressed as
anomalies based on 1961 — 1990 temperature averages (b); changes in ENSO - related variability based on El Junco diatom record [41], oxygen isotopes records from Palmyra [42], and the unified ENSO proxy [UEP; 23](c); changes in PDSI variability for the American Southwest (d), and changes in winter
precipitation variability as simulated by CESM model ensembles 2 to 5 [43].