or experienced terms, for
only a minority of individuals. One possible implication of this is pointed out by
Eiser (2004) who argues that a lack of a directly experienced link between the
causes of climate change and its consequences may be creating a false impression
that activities which lead to dangerous outcomes are in fact safe. Similar findings
emerge from a survey of a representative sample
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
towards the northern part of Vatnajökull.
Table 8 – Median 1M5 values (mm 24-h-1) for eleven hydropower catchments with and
without climate projections for the period 2080 – 2100.
Catchment
1M5 median value
mm 24-h-1
Original
RCP 2.6 RCP 8.5
10% 50% 90% 10% 50% 90%
Blönduvirkjun 48 41 49 58 42 50 61
Búðarháls 46 40 47 56 40 48 59
Hágöngulón 63 55 65 76 55 66 81
Hálslón 85 75 88 104
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
.................... 85
8
Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86
Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87
Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88
Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
2015. For an updated graph, see link in main text.
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/about-imo/news/bigimg/3203
characterized by two dif-
ferent management paradigms—management as control
versus management as learning—are contrasted as the
extreme, opposing ends of six axes.
Interdependence of the regime characteristics
and responsiveness to floods and droughts
The key objective of our research is to see whether there is
a link between regime characteristics and responsiveness to
floods and droughts (as an output
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf