240 likes | 251 Views
This article provides an overview of the current drought status in Kansas, including the November Palmer Index, moisture conditions, precipitation outlook, and drought outlook. It also discusses the reasons for the drought, including the effects of La Niña, changes in North Atlantic Oscillation, and changes in Arctic Oscillation.
E N D
Drought 2011: Where are We and What’s Next? Kansas Winter Grazing Conference June 10, 2014
Current Drought Status K-State Research & Extension
Kansas Drought Status K-State Research & Extension
November Palmer Index K-State Research & Extension
Moisture Needed K-State Research & Extension
Moisture Needed K-State Research & Extension
Typical January Moisture K-State Research & Extension
What’s the Precipitation Outlook? K-State Research & Extension
What’s the Precipitation Outlook? K-State Research & Extension
What’s the Precipitation Outlook? K-State Research & Extension
Vegetative Conditions K-State Research & Extension
What’s the Drought Outlook? K-State Research & Extension
What’s the Drought Outlook? K-State Research & Extension
Why? Continuing La Niña Change in North Atlantic Oscillation Change in Artic Oscillation K-State Research & Extension
North Atlantic Oscillation The North Atlantic Oscillation (NAO). When the NAO index is low, shown above, ocean winds are weaker and the U.S. winter more severe. Changes in ocean temperature distributions are also observed. Its "high index" state corresponds to particularly high atmospheric pressure over the Azores, an intense low over Iceland. Ocean winds are stronger and winters milder in the eastern U.S. (Illustration by Fritz Heide & Jack Cook, WHOI) http://www.whoi.edu/page.do?pid=12455&tid=282&cid=10146
Mary Knapp Weather Data Library 1703 Throckmorton Hall Kansas State University Manhattan, KS 66506 PH: 785 532-7019 E-mail: Mknapp@ksu.edu URL: http://www.ksre.ksu.edu/wdl K-State Research & Extension