WEATHER CONDITIONS IN THE EAST OF NORWAY
by Knut Jørgen Røed Ødegaard and Unni Fuskeland
In the south of Norway, May 31. is early summer. But the temperatures
and the weather may change a lot from one year to another.
Even so, the air is in general dryer than later in the summer, and this
results in less rain and clouds and some years in longer periods with heat and
drought.
Observations done at Jevnaker (145 meter above sea level) may be an example
of the conditions in the central part of the southeast of Norway in
May/June:
|
Year
|
Min. temp
|
Max. temp
|
Rain/weather
|
Comments
|
| 2002 |
4,5 |
17,5 |
4,3 mm/showers |
Right before a hot periode |
| 2001 |
6 |
16 |
dry spell |
Rain the day before (showers) |
| 2000 |
5 |
17 |
insignificant/showers |
|
| 1999 |
7 |
20,5 |
dry spell |
Long periode with nice weather (b. 05.29.) |
| 1998 |
7,5 |
22,5 |
dry spell |
Nice periode |
| 1997 |
7 |
22 |
dry spell |
Start of a hot periode |
| 1996 |
8 |
14,5 |
9,8 mm/area,showers |
Storm in the west, nice before and especially after |
| 1995 |
11 |
18 |
12,4 mm/area,showers |
Large flooding in eastern Norway |
| 1994 |
7 |
18 |
dry spell |
Storm in the middle of Norway |
| 1993 |
8,5 |
18,5 |
10,9 mm/area,showers |
|
| 1992 |
8 |
29 |
dry spell |
Middle of a long dry periode |
| 1991 |
5 |
17 |
dry spell |
End of a long dry periode |
| 1990 |
7 |
20 |
insignificant/area |
Rather nice periode |
| 1989 |
1 |
7 |
5,0 mm/area |
|
| 1988 |
6,5 |
22 |
insignificant/thunder |
Unstable period |
| 1987 |
6 |
12,5 |
insignificant/showers |
Probably clouds |
| 1986 |
1 |
18,5 |
dry spell |
Nice periode |
| 1985 |
4,5 |
23 |
dry spell |
Periode with really nice weather |
| 1984 |
9,5 |
21 |
dry spell |
Nice periode |
| 1983 |
5 |
21 |
insignificant/showers |
|
| 1982 |
- |
Over 20 |
dry spell |
Nice periode |
The minimum temperatures will in general be higher in Oslo and in areas
near the coast, and the maximum temperatures somewhat lower the farther north.
When rain comes from a precipitation area, it indicates
a long term, continuous cover of clouds.
A great deal of the rain comes as showers in the afternoon. These clouds
are caused due to heating of the Sun during the day. In general the same
heating causes a decreased cover of clouds in the afternoons.
Since the eclipse happens early in the morning, these kinds of clouds will
not have been created.
|
|
Thunder clouds in the east of Norway on August 16. 2003.
Photo: Oddleiv Skilbrei
|
CONTACT PERSON:
Knut Jørgen Røed Ødegaard
Project leader
Institute of Theoretical Astrophysics
P.O.Box 1029 Blindern
N-0315 Oslo
Norway
Phone: +47 22 85 75 22 (Institute of Theoretical Astrophysics)
+47 992 77 172 (mobile phone)
+47 613 11 359 (private, weekend)
Email: knutjo@astro.uio.no
Created 24.03.03, modified 28.03.03 by Unni Fuskeland
Address: webmaster@astro.uio.no |