exploitation and strict management of domestic natural
resources, paying less attention to environmental consequences,
for example through the institutionalisation of the Water Security
Framework. Towards 2030, climate change becomes an issue,
triggering new sets of conicts. These are resolved by strong EU
leadership and the newly formed border police, or otherwise
neutralised by the fear
/media/loftslag/Kok_et_al._TFSC_published_2011.pdf
8 9 NA
Height of 1st cloud layer
Number of record
s
Station
Manual
Automatic
Figure 2. Number of records as a function of the height of the 1st cloud layer.
Figure 3 shows automatic records as a function of manual observations without the NA’s, con-
taining 1263 concurrent records. In 86% cases the automatic station gives a higher value than
the manual one; most frequently one height interval (h
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
on Climate
Change (IPCC) report states that global atmospheric con-
centrations of greenhouse gases (GHG) have increased
markedly since 1750 as a result of human activities
[Intergovernmental Panel on Climate Change (IPCC),
2007]. IPCC predicts that GHG concentrations will continue
to rise during the present century at rates determined by
global economic development with significant impacts
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
with vertical boundary-layer profiles calculated di-
rectly from HARMONIE model levels. Due to the temporal and spatial variability of model
level heights, for the calculation of average vertical profiles, individual model profiles above
6The large positive bias northeast of Vatnajökull is due to the unusually cold summertime temperatures measured
at Station 5932, situated near the edge
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
–2015. This summer, 2021, a
conversion code was developed that converts these archaic, binary tremlogs to a standardized
csv format, which can be plotted with any type of meteorological or volcano monitoring data,
including gas measurements, number of earthquakes, rainfall measurements, etc. This con-
version of data was vital for tuning the ALERT module and may be very useful for further
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
wetland, and for
moving the entire wellfield to another location. There is
also the problem of occasional flooding. Three BNs were
constructed for: flooding, afforestation and farming con-
tracts. However, the focus of the present paper is restricted
to the BN dealing with farming contracts.
Interference with the final BN documented that com-
pensation payment must be in the highest state
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
with the same method used to estimate
qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the
estimation is made individually for each site i by pooling AMF series for different durations D.
The index flood, µi(D), is modelled at each site i as a continuous function of D, as follows:
12
µi(D) =
µi
1+(D=Di)li
; (6)
where µi, Di and li are basin dependent parameters
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
The IFM was evaluated assuming that the target site was totally ungauged. A cross-validation
strategy was developed. Each of the twelve gauged sites presented in Fig. 1 was in turn con-
sidered as the ungauged "target" site i for which flood quantiles were required. The IFM was
recursively developed without using the AMF data from that site, and then used to infer the in-
dex flood (µi(D)) and flood
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf