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• Microsoft Word - MetO_Atlantic_tropical_storm_forecast_verification_1Dec2013_v0.doc

  region were indeed neutral (i.e. tropical Pacific sea surface temperatures, sea level pressure, cloudiness and trade winds indicated that neither El Niño nor La Niña conditions were present; WMO 2013). Furthermore, cool SST anomalies were also present in the far eastern Pacific, although they were

• wiser-mena-scoping-study-external-v2.pdf

  and statistical forecasts into a reproducible, objective procedure that is verifiable is the seasonal forecasting approach recommended by WMO (2020). 12 The NAO represents variability in sea-level pressure (SLP) in the North Atlantic. In the average state of the atmosphere, the North Atlantic surface

• trd---climate-risk-report-for-csa---v4-final.pdf

  between June-September. ENSO involves recurrent changes in sea surface temperatures and atmospheric surface pressure across central and eastern tropical Pacific. ENSO has three phases: El Niño, La Niña, and neutral. El Niño generally suppresses monsoon rainfall while La Niña generally increases

• trd---climate-risk-report-for-csa---v4-final-april-2026pdf

  seasonal rainfall occurring between June-September. ENSO involves recurrent changes in sea surface temperatures and atmospheric surface pressure across central and eastern tropical Pacific. ENSO has three phases: El Niño, La Niña, and neutral. El Niño generally suppresses monsoon rainfall while La Niña

• trd---climate-risk-report-for-csa---v4-final-april-2026.pdf

  seasonal rainfall occurring between June-September. ENSO involves recurrent changes in sea surface temperatures and atmospheric surface pressure across central and eastern tropical Pacific. ENSO has three phases: El Niño, La Niña, and neutral. El Niño generally suppresses monsoon rainfall while La Niña

• trd---climate-risk-report-for-sea---v2-final.pdf

  of the dateline. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called the Southern Oscillation. This coupled atmosphere–ocean phenomenon, with preferred time scales of two to about seven years, is known as the El Niño- Southern

• trd---climate-risk-report-for-sea---v2-final-april-2026.pdf

  of the tropical Pacific Ocean east of the dateline. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called the Southern Oscillation. This coupled atmosphere–ocean phenomenon, with preferred time scales of two to about seven years

• trd---climate-risk-report-for-sea---v2-final-april-2026pdf

  of the tropical Pacific Ocean east of the dateline. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called the Southern Oscillation. This coupled atmosphere–ocean phenomenon, with preferred time scales of two to about seven years

• southern-africa-climate-risk-report-trd-finalpdf

  since become identified with warming of the tropical Pacific Ocean east of the dateline. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called the Southern Oscillation. This coupled atmosphere–ocean phenomenon, with preferred

• southern-africa-climate-risk-report-trd-final.pdf

  since become identified with warming of the tropical Pacific Ocean east of the dateline. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called the Southern Oscillation. This coupled atmosphere–ocean phenomenon, with preferred