cumulative levels of precipitation over a 1-hour, 3-hour or 6-hour period, depending on the forecast length.
The colour scale denotes precipitation rates, from light precipitation of 0.1 mm/hour (0.3 mm/3 hours and 0.5 mm/6 hours) shown in light yellow, up to heavy precipitation of 50 mm/hour (90 mm/3 hours and 200 mm/6 hours) shown in red.
Wind barbs are also shown on the maps. The stem of the barb
/weather/articles/nr/1211
and their interactions with sustainable develop-
Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages.
Schematic framework of anthropogenic climate change drivers, impacts and responses
ment. Topic 5 assesses the relationship between adaptation and
mitigation on a more conceptual basis and takes a longer-term per-
spective. Topic 6/media/loftslag/IPPC-2007-ar4_syr.pdf
................................................................................................................. 45
6 DISCUSSION ...................................................................................................................... 49
6.1 Differences in return levels between observed and simulated precipitation ..................... 49
6.2 Sensitivity of the EVA methods
/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
to increase in Finland by 13–26% by the 2080s (Ruosteenoja
and Jylhä, 2007) and extreme precipitations are expected to in-
crease (Beniston et al., 2007). On the other hand, temperature in-
creases of 2–6 C by the end of the century are estimated to
decrease the snow accumulation by 40–70% by the same period
(Vehviläinen and Huttunen, 1997; Beldring et al., 2006; Ruosteeno-
ja and Jylhä, 2007
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
a coherent, emergent signal in RSAM data (see Figure
2), raising the question: Can RSAM data be empirically used to detect volcanic tremor events
preceding eruptions?
6
Figure 1. Photo of the monitoring setup in the IMO’s natural hazards monitoring room. The
right screen shows real-time earthquake and tremor data. Tremv output is displayed in red
box with the last 24 hrs of all frequency
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
of the rifting event. They were shallow,
low-frequency and had unusual focal mechanisms. At the end of
2014, this activity had decreased significantly and since the end of
February 2015 only small earthquakes have been recorded in the
area.
Photo: Elín Björk Jónasdóttir.
6
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
Monitoring gas emission and
environmental
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf