Skip Navigation Links www.nws.noaa.gov 
NOAA logo - Click to go to the NOAA home page National Weather Service   NWS logo - Click to go to the NWS home page
Climate Prediction Center

 
 

Climate Diagnostics Bulletin
Climate Diagnostics Bulletin - Home Climate Diagnostics Bulletin - Tropics Climate Diagnostics Bulletin - Forecast

 

  Extratropical Highlights

  Table of Indices  (Table 3)

  Global Surface Temperature  E1

  Temperature Anomalies (Land Only)  E2

  Global Precipitation  E3

  Regional Precip Estimates (a)  E4

  Regional Precip Estimates (b)  E5

  U.S. Precipitation  E6

  Northern Hemisphere

  Southern Hemisphere

  Stratosphere

  Appendix 2: Additional Figures

Extratropical Highlights

DECEMBER 2017

1

Extratropical Highlights –December 2017

 

1. Northern Hemisphere

The 500-hPa circulation during December featured an anomalous wave-4 pattern. Above-average heights were present over the western North Pacific, western North America, the eastern North Atlantic, and northwestern Russia. Below-average heights were present over the central North Pacific, Hudson Bay, Scandinavia, and eastern Asia (Fig. E9).

At 200-hPa, the circulation featured amplified troughs east of the date line in the subtropics of both hemispheres (Fig. T22).  This pattern is typical of La Niña, and reflects the disappearance of deep tropical convection from the central equatorial Pacific.

The main land-surface temperature signals during December included above-average temperatures in Alaska, northwestern Canada, and western Russia, and below-average temperatures in the U.S. Great Lakes region (Fig. E1). The main precipitation signals included above-average totals in western Russia, and below-average totals in western Canada and in the southwestern and central/ eastern portions of the U.S. (Fig. E3).

 

a. North Pacific and North America

The 500-hPa circulation during December featured above-average heights over western North America and below-average heights over eastern North America. Highly amplified wave patterns such as this often reflect the westward retraction of the East Asian jet steam typically seen during La Niña (Fig. T21).

This overall pattern contributed to anomalously warm conditions in Alaska, western Canada, and the southwestern U.S., and to anomalously cool conditions in the U.S. Great Lakes region (Fig. E1). It also contributed to below-average precipitation in western North America and across the central/ eastern portions of the U.S. (Fig. E3).

 

b. Eurasia

            An amplified wave pattern at 500-hPa extended from the eastern North Atlantic to eastern Asia (Fig. E9). Features of this pattern included an amplified ridge over the eastern North Atlantic and a strong tough extending southward from Scandinavia. This pattern was associated with well above-average surface temperatures (Fig. E1) and above-average precipitation across eastern Europe and western Russia (Fig. E3).

 

2. Southern Hemisphere

The mean 500-hPa circulation during December featured above-average heights in the vicinity of New Zealand and below-average heights over much of the high latitudes (Fig. E15). At 200-hPa the circulation featured an amplified trough over the east-central South Pacific Ocean (Fig. T22),  which is typical of La Niña.

 


NOAA/ National Weather Service
NOAA Center for Weather and Climate Prediction
Climate Prediction Center
5830 University Research Court
College Park, Maryland 20740
Page Author: Climate Prediction Center Internet Team
Page Last Modified: January 2018
Disclaimer
Information Quality
Credits
Glossary
Privacy Policy
Freedom of Information Act (FOIA)
About Us
Career Opportunities