Temperature and precipitation variations in Norway 1900-1994 and their links to atmospheric circulation

International Journal of Climatology

Volumn 20, Issue 14, 2000, Pages 1693-1708

  Hanssen Bauer, Inger ^a   Førland, Eirik ^a  

^a NORWEGIAN METEOROLOGICAL INSTITUTE   (Norway)

Author keywords

Atmospheric circulation; Early 20th century warming; Precipitation trends; Temperature trends

Indexed keywords

ATMOSPHERIC CIRCULATION; DECADAL VARIATION; PRECIPITATION (CLIMATOLOGY); SEA LEVEL PRESSURE; TEMPERATURE; TREND ANALYSIS;

NORWAY;

EID: 0034506433     PISSN: 08998418     EISSN: None     Source Type: Journal    
DOI: 10.1002/1097-0088(20001130)20:14<1693::AID-JOC567>3.0.CO;2-7     Document Type: Article

References (21)

1. A homogeneity test applied to precipitation data
2. Changes in atmospheric circulation over Northern Hemisphere oceans associated with the rapid warming of the 1920s
3. Downscaling of temperature and precipitation in Norway based upon multiple regression of the principal components of the SLP field
4. Homogenizing long Norwegian precipitation series
5. Annual and seasonal precipitation variations in Norway 1896-1997
6. Long-term trends in precipitation and temperature in the Norwegian Arctic: Can they be explained by changes in atmospheric circulation patterns?
7. Annual and seasonal temperature variations in Norway 1876-1997
8. Estimating regional precipitation trends-comparison of two methods
9. Decadal trends in the North Atlantic Oscillation: Regional temperatures and precipitation
10. An intercomparison of computer-assisted circulation classification methods
11. Regional climate under global warming
12. The early twentieth century Arctic high-fact or fiction?
13. Climate response to increasing levels of greenhouse gases and aerosols
14. Global and regional climate in 1998
15. Detection of climate change and attribution of causes
16. Climatological network design
17. Climate instability determination. Discussion of methods and examples
18. Causes of twentieth century temperature change near the earth's surface
19. A shift in the NAO and increasing storm track activity over Europe due to anthropogenic greenhouse gas forcing
20. Interannual variability of central European mean temperature in January-February and its relation to large-scale circulation