that flowed around the gauging location.Updated 6.9. 13:45According to the latest measurements, floodwater from the eastern cauldron will reach Sveinstindur this evening, 6 September. Based on previous examples, it is likely that the flood from the eastern cauldron will peak at Sveinstindur about 30 hours after first being detected there. By Wednesday morning, 7 September, the flood front will have
/about-imo/news/flood-in-estern-skafta
that flowed around the gauging location.Updated 6.9. 13:45According to the latest measurements, floodwater from the eastern cauldron will reach Sveinstindur this evening, 6 September. Based on previous examples, it is likely that the flood from the eastern cauldron will peak at Sveinstindur about 30 hours after first being detected there. By Wednesday morning, 7 September, the flood front will have
/about-imo/news/flood-in-estern-skafta/
An
article recently published in the journal Frontiers in Earth Science on
glacier changes in Iceland describes changes in the volume and mass of the Icelandic
glaciers since they reached historical maximum extent at the end of the
so-called Little Ice Age shortly before 1900. The results of a number of
studies covering about 99% of the glacier area are summarized
/about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years
Reassessment of precipitation
return levels in Iceland
Andréa-Giorgio R. Massad, Guðrún Nína Petersen, Tinna
Þórarinsdóttir, Matthew James Roberts
VÍ 2020-008
Skýrsla
Reassessment of precipitation return
levels in Iceland
VÍ 2020-008
ISSN 1670-8261
Skýrsla
+354 522 60 00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Andréa-Giorgio R. Massad, Guðrún Nína Petersen, Tinna
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
Ísskýsla 7.apríl
Flug 03410.025
Miðvikudaginn 7 apríl var farið í ískönnunarflug á TF-SIF úti fyrir vestfjörðum. Kl.1115
var komið að ísröndini sem lá til NA um eftirtalda staði:
1. N65°50'- W028°05'
2. N65°44' -W027°49 '
3. N65°56'- W027°08'
4. N66°12' -W026°21'
5. N66°31'- W025°57'
6. N66°43'- W025°49'
7. N66°40'- W025°24'
8. N67°05'- W024°32'
9. N67°14' -W023°56'
10.N67°19'- W023°32'
11.N67°40
/media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf
0
50
0
J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D
J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D
J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D
2010–39(a)
0
10
0
20
0
30
0
40
0
50
0
2040–69(b)
Lake Pielinen
0
10
0
20
0
30
0
40
0
50
0
2070–99(c)
0
1
0
3
0
5
0
7
0
2010–39(d)
0
1
0
3
0
5
0
7
0
2040–69(e)
Lake Syväri
0
1
0
/media/ces/Water_resources_man_Veijalainen_etal.pdf
164
Keflavíkurflugvöllur
1081.6
98
99
41.9
226
157
The annual
total precipitation in Reykjavík was 1062.4 mm, 20% above the 1991
to 2020 average precipitation. In Akureyri the total was 600.9 mm, 5%
above the 1991 to 2020 mean.The
number of days with precipitation equal to or exceeding 1.0 mm, were
156 in Reykjavík, 7 more than the mean 1991 to 2020
/about-imo/news/the-weather-in-iceland-in-2022
in
Neskaupsstaður in the East on 13 August. The lowest minimum -28.3°C
was measured at Setur (located in the Highlands) on 7 March. The
lowest minimum in inhabited areas, -28.1°C was measured at Mývatn
in the Northeast on 13 February.The
absolute maximum in Reykjavík was 21.4°C, recorded on 21 and 29
June and the absolute minimum was -10.0°C on 19 November. In
Akureyri the maximum was 23.5°C
/about-imo/news/the-weather-in-iceland-in-2020