Lifandi kennslu stofa í lolags breytingumA natural laboratory to study climate change
Jöklar ÍslandsIcelandic glaciers
Yrlit um íslenska jökla í árslok
Jöklar á Íslandi hafa hopað hratt í rúma tvo áratugi og er rýrnun þeirra einhver helsta aeiðing hlýnandi loslags hérlendis og skýr vitnis burð-
ur um hlýn un ina. Hér er gerð stutt grein fyr ir breytingum á jökl un um síðan um aldamótin
/media/Eplicanámskeið/VAT_newsletter_2018_06.pdf
and a true friend - always ready to help, whether the problem involved deciphering convoluted computer codes, delving into the mysteries of the SIL system, making presentable documents using LaTeX, or discussing life, the universe and everything.
Publications
Sigurður Th. Rögnvaldsson
Sigurður Th. Rögnvaldsson, Gylfi P. Hersir og Knútur Árnason 1987. Viðnámsmælingar, fræðileg úttekt, mæling og/earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/
and a true friend - always ready to help, whether the problem involved deciphering convoluted computer codes, delving into the mysteries of the SIL system, making presentable documents using LaTeX, or discussing life, the universe and everything.
Publications
Sigurður Th. Rögnvaldsson
Sigurður Th. Rögnvaldsson, Gylfi P. Hersir og Knútur Árnason 1987. Viðnámsmælingar, fræðileg úttekt, mæling og/earthquakes-and-volcanism/conferences/jsr-2009/sigurdur
indicate that
inhabited regions might be exposed to heavy tephra fallout. In the light of this outcome it is
recommended that exposed regions have in place plans to implement regular roof cleaning to
avoid accumulation of critical load potentially causing collapse and damages to house and
buildings.
11
Ágrip
Eldgos eru margvísleg og geta þróast á mismunandi hátt. Í sprengigosi
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
Hafísskýrsla TF-SIF
11. maí 2011
Flug nr. 03511.025
Ískönnunarflug 11. maí 2011
Í dag var farið í ískönnunarflug um vesturmið. Enginn hafís var sjáanlegur í íslenskri lögsögu,
en þéttur hafís rétt inn þeirrar grænlensku. Gerðum hafískönnun með SLAR ratsjá og ELTA
eftirlitsratsjá. Skyggni á svæðinu leifði ekki athugun með berum augum. Hér að neðan fylgir
punktalisti yfir legu
/media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf
Reykjavík 23. mars 2011.
Til:Veðurstofu Íslands.
Frá: Landhelgisgæslu Íslands.
Efni: Hafískönnun 23 mars 2011.
Miðvikudaginn 23. mars 2011 fór þyrla Landhelgisgæslunar í ísleiðangur og var flogið norður
með Vestfjörðum. Komið var að ísröndinni út af Látrabjargi og henni fylgt til norðausturs um
eftirfarandi staði.
1. 65°50N 026°56V
2. 66°08N 026°26V
3. 66°16N 026°22V
4. 66°22N 025
/media/hafis/skyrslur_lhg/hafisskyrsla-23-mars-2011.pdf
line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000
in 1991. The blue dashed line shows the number of all measured earthquakes
but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the
reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm
/media/jar/Bardarbunga-2014_August-events.pdf
line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000/