REYKJAVÍK, ICELAND AUGUST 11-13, 2008 - Veðurstofa Íslands

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PLENARY SESSION 1 <strong>11</strong>
Page 1 and 2: NORTHERN HYDROLOGY AND ITS GLOBAL R
Page 3 and 4: NORTHERN HYDROLOGY AND ITS GLOBAL R
Page 5 and 6: LIST OF CONTENTS VOLUME 1 Preface .
Page 7 and 8: Session 4: Uncertainty And Extremes
Page 9 and 10: Astrid Voksø: Using Gis To Calcula
Page 11: PREFACE This is the fifth Nordic Hy
Page 16 and 17: e complete and exhaustive in record
Page 18 and 19: society issues the journal Jökull,
Page 20 and 21: and for nationwide mapping as well
Page 22 and 23: supported by the Nordic Council of
Page 24 and 25: series on hydropower development, i
Page 26 and 27: • as individual experts recruited
Page 28 and 29: attempts at quantification indicate
Page 30 and 31: Lemmelä, R. and Helenius, N., eds.
Page 32 and 33: Non-exhaustive list of selected maj
Page 34 and 35: CLIMATE CHANGE AND VARIABILITY: HOW
Page 36 and 37: URBAN HYDROLOGY AND SUSTAINABLE URB
Page 38 and 39: This paper describes the stormwater
Page 40 and 41: The table 2 shows a great differenc
Page 42 and 43: Table 4. Efficiency in treating sto
Page 44 and 45: particles and binding dissolved mat
Page 46 and 47: Stahre, P., 2006. Sustainability in
Page 49 and 50: CHANGES IN ICE REGIMES OF RIVERS IN
Page 51 and 52: events decreased by 5-15% and the d
Page 53 and 54: Ice cover duration, days 200 180 16
Page 55 and 56: The observed thinning of the maximu
Page 57 and 58: other important Arctic science init
Page 59 and 60: THE PROBLEM OF DECLINING NETWORKS A
Page 61 and 62: comprehensive pan-Arctic observatio
Page 63 and 64:
2002; Hinzman et al.; 2005, Walsh e
Page 65 and 66:
Values 2-4 indicate that one to thr
Page 67 and 68:
difficult to determine the real vul
Page 69 and 70:
POTENTIAL IMPACT OF CLIMATE CHANGE
Page 71 and 72:
MATERIALS AND METHODS Location The
Page 73 and 74:
PROMES (Universidad Complutense de
Page 75 and 76:
RESULTS Validation of the present s
Page 77 and 78:
Figure 4. The effect of climate cha
Page 79 and 80:
global warming seems to accelerate
Page 81 and 82:
Calanca, P. Roesch, A. Jasper, K. W
Page 83 and 84:
Swift, DA. Nienow, PW. Hoey, TB. Ma
Page 85 and 86:
temperature can determine the fate
Page 87 and 88:
RESULTS AND DISCUSSIONS Meteorologi
Page 89 and 90:
June just prior to summer stratific
Page 91 and 92:
Figure 5. Vertical temperature prof
Page 93 and 94:
Figure 6. Monthly average a) water
Page 95 and 96:
REFERENCES Andradóttir, H.O, and N
Page 97 and 98:
These jökulhlaups are of the rapid
Page 99 and 100:
The distance from the glacier snout
Page 101 and 102:
front of the flood wave between the
Page 103 and 104:
REFERENCES Björnsson, H. 1992. Jö
Page 105 and 106:
The objective of the present study
Page 107 and 108:
COMPARISON OF OBSERVED WEATHER DATA
Page 109 and 110:
Daily streamflow simulation The qua
Page 111 and 112:
Annual discharge In the final compa
Page 113 and 114:
ACKNOWLEDGEMENT The research report
Page 115 and 116:
ICE AND WEATHER CONDITIONS IN THE G
Page 117 and 118:
Ice processes can be described acco
Page 119 and 120:
thous.km2 450 400 350 300 250 200 1
Page 121 and 122:
SOME METEOROLOGICAL PARAMETERS IMPA
Page 123 and 124:
TOWARDS INTEGRATED SYSTEMS FOR ARCT
Page 125 and 126:
other hand, small scale process stu
Page 127 and 128:
In 2000, Malin and Edgett published
Page 129 and 130:
Icelandic gullies vary in cross-sec
Page 131 and 132:
gullies than others. Similarly, geo
Page 133 and 134:
assumed to be on the order of 10,00
Page 135 and 136:
SESSION 3: WATER RESOURCES MANAGEME
Page 137 and 138:
LONG-TERM RECORDS OF PRECIPITATION
Page 139 and 140:
8 6 4 2 0 -2 -4 -6 Ainazi Gulbene K
Page 141 and 142:
100 80 60 40 20 0 -20 -40 -60 -80 A
Page 143 and 144:
series for most of the stations sho
Page 145 and 146:
CLIMATE CHANGE AND POLLUTION RISKS
Page 147 and 148:
At the airport Propylene glycol (PG
Page 149 and 150:
water samples at different depths w
Page 151 and 152:
Normalised annual consumption of de
Page 153 and 154:
B Figure 6. Scenario results of Cl
Page 155 and 156:
Proceedings of the Geological Socie
Page 157 and 158:
ased on several regional regression
Page 159 and 160:
% lowest part and the 15 % highest
Page 161 and 162:
Figure 2. Catchment characteristic
Page 163 and 164:
therefore it is interesting to exam
Page 165 and 166:
19 20 5 21 11 25 22 6 7 8 2 4 0 50
Page 167 and 168:
annual maximum water level often oc
Page 169 and 170:
500 400 300 200 100 Discharge (m 3
Page 171 and 172:
discharges and low flows have decre
Page 173 and 174:
CLIMATE CHANGE IMPACTS ON THE TOTAL
Page 175 and 176:
perspective associated with signifi
Page 177 and 178:
The study period from 1988 to 2006
Page 179 and 180:
Similar results were obtained to an
Page 181 and 182:
The higher ration was fond for the
Page 183 and 184:
CONCLUSIONS The present results con
Page 185 and 186:
INTRODUCTION The potential impacts
Page 187 and 188:
Table 1. HBV parameter ranges used
Page 189 and 190:
Percentage at or below given value
Page 191 and 192:
scenarios for this catchment. The s
Page 193 and 194:
OVERLAND FLOW INDUCED BY SNOWMELT,
Page 195 and 196:
Sweden, the University of Minnesota
Page 197 and 198:
Figure 1. Overland flow in the Skut
Page 199 and 200:
Figure 3. Measured and calculated h
Page 201 and 202:
Deelstra, Johannes, Sigrun H. Kvær
Page 203 and 204:
and Jauja, 1999), METQ2005 and METQ
Page 205 and 206:
Daily meteorological data were used
Page 207 and 208:
Discharge (m 3 /s) 110 100 90 80 70
Page 209 and 210:
locates in the middle part of the R
Page 211 and 212:
Seibert, J. 1999. Regionalization o
Page 213 and 214:
power. Dams, built for water storag
Page 215 and 216:
INTRODUCTION Background Due to the
Page 217 and 218:
In the beginning planners and engin
Page 219 and 220:
involved. This is to avoid unnecess
Page 221 and 222:
Thorolfsson, S. T., Aasen, A., Seks
Page 223 and 224:
SESSION 4: UNCERTAINTY AND EXTREMES
Page 225 and 226:
DOWN-SCALING ATMOSPHERIC PATTERNS T
Page 227 and 228:
information. However, in NHMMs the
Page 229 and 230:
As shown in (6), the two terms summ
Page 231 and 232:
Figure 2. Precipitation mean amount
Page 233 and 234:
Pr[ Spell duration ≥ days ] Pr[ S
Page 235 and 236:
0 0.25 0.5 0.75 1 Geopotential heig
Page 237 and 238:
Bellone, E., Hughes, J. P. and Gutt
Page 239 and 240:
distribution, especially in the dat
Page 241 and 242:
y initial and boundary data from th
Page 243 and 244:
Figure 3: Estimated mean accumulate
Page 245 and 246:
372, and the greatest skill on Brú
Page 247 and 248:
Effect of climate change on hydrolo
Page 249 and 250:
downscaled for the period 1961-2006
Page 251 and 252:
flows from the SE (not shown). The
Page 253 and 254:
Figure 5: Ratio [%] of "missing" ev
Page 255 and 256:
Figure 7: Measured and simulated (W
Page 257 and 258:
Benoit, R., Pellerin P., Kouwen N.,
Page 259 and 260:
e directly used in impact models, s
Page 261 and 262:
The method to scale RCM precipitati
Page 263 and 264:
future scenario precipitation. The
Page 265 and 266:
Figure 4. Distribution of daily tem
Page 267 and 268:
Erik Kjellström, E., Bärring, L.,
Page 269 and 270:
Numerous studies have explored the
Page 271 and 272:
theoretical L-moment ratios with th
Page 273 and 274:
Eight Norwegian gauging stations ha
Page 275 and 276:
frequency analysis are not easy to
Page 277 and 278:
ESTIMATING BAYESIAN RATING CURVES F
Page 279 and 280:
See Petersen-Øverleir (2004) og Mo
Page 281 and 282:
Figure 1. The estimate of maximum a
Page 283 and 284:
the Bayesian approach described abo
Page 285 and 286:
Figure 5. The same rating curves as
Page 287 and 288:
[7] Árnason, S., 2008. The estimat
Page 289 and 290:
lines were damaged by this storm. T
Page 291 and 292:
highest observed water level. Lake
Page 293 and 294:
Figure 2. Empirical (filled dots) a
Page 295 and 296:
magnitude of the fluctuations water
Page 297 and 298:
EXTREME RAINFALLS AND DAMAGES ON AU
Page 299 and 300:
RAINFALL MEASUREMENTS The short-ter
Page 301 and 302:
Trondheim Radar Nidelva =83,4 l/s·
Page 303 and 304:
highest intensity at Risvollan with
Page 305 and 306:
study were that the cost for this m
Page 307 and 308:
305 Figure 1. The main phases of th
Page 309 and 310:
esults to be meaningful careful pre
Page 311 and 312:
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Page 313 and 314:
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Page 315 and 316:
300 280 260 240 220 200 180 ��
Page 317 and 318:
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Page 319:
p(b) ∝Æ(b|µb = 2.15, σ 2 b = 0
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REYKJAVÍK, ICELAND AUGUST 11-13, 2008 - Veðurstofa Íslands

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