News
03/29/2022, 11:35 am EDT

Dryness Returns to Wheat-growing Areas of East China

Late calendar winter was dry in East China wheat-growing areas raising concern regarding drought. However, due to presence of the Madden Julian oscillation in the far western Pacific during the past 10 days a wetter regime eased the dryness. New week 2-4 forecasts reveal the dryness returns!
03/28/2022, 4:50 am EDT

Europe/Western Russia/Black Sea Region Turns Colder and Stormy for Early April

This week, a transition to a sharp negative phase of the Scandinavia Index takes place. During -SCAND, an upper trough becomes dominant across northwest Eurasia. Initially, temperatures turn quite cold across Northern Europe/Northwest Russia featuring some arctic air. In the 6-10-day period the upper trough elongates into Southwest Europe and the attendant chill expands across all of Europe reaching Ukraine and Western Russia.
03/21/2022, 12:25 pm EDT

At The Surface La Nina Has Weakened. However, Subsurface Diagnostics Indicate Strengthening!

A transient (warm) Kelvin Wave traversing the equatorial Pacific during late meteorological winter in the northern hemisphere warmed the East Pacific and caused La Nina to weaken. However, the Kelvin Wave is constricting and the East Pacific subsurface beneath the equator is cooling again. expect La Nina to regain strength into April.
03/17/2022, 2:28 pm EDT

Explaining What Caused The Western Europe Dust Storm

The past couple days brought a northward surge of dust from the Sahara Desert to Southwest Europe reaching U.K. Dust storms over Southwest Europe are not unusual this time of year. However, the northern expanse and intensity of this event was exceptional. The northern surge of Sahara Dust was caused by a strong low-level southerly current of air across Northwest Africa in-between a small but potent upper trough on the Northwest Coast of Africa and an amplified upper ridge pattern over Northern Europe. The pattern is characteristic of the positive phase of the Scandinavia Index (+SCAND) regime.