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1 Spatial Modelling of the Terrestrial Environment - Georeferencial

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270 Index<br />

floodplain maps, UK 92<br />

flow velocity 85<br />

form drag 86–7<br />

friction data, spatially distributed 94–5<br />

benchmark validation dataset 94–5<br />

friction, in hydraulic models 86–92<br />

skin friction for in-channel flows 87<br />

vegetation biophysical attributes 88–92<br />

vegetation classification 87–8<br />

gauging stations, national spacing defined by flood<br />

warning role 81–2<br />

Geosat 17<br />

Geostationary Operational <strong>Environment</strong>al Satellites<br />

(GOES:US)<br />

GOES Precipitation Index (GPI) 162<br />

remotely sensed FRE from 191, 192<br />

GEWEX Global Soil Wetness Project 251<br />

GIS 3, 4, 264<br />

integrated, and policy measures 241–2<br />

and remote sensing, in fire modelling 112<br />

see also SHIRE 2000 GIS<br />

Glen’s flow law 15, 20<br />

and diagnostic velocities 26<br />

Global Data Assimilation System (GDAS), wea<strong>the</strong>r<br />

forecast model 251<br />

GOES Precipitation Index (GPI) 162<br />

gravitational driving force, and ice sheet dynamics<br />

14–15, 30<br />

Gravity Recovery and Climate Experiment (GRACE)<br />

253–4<br />

Greenland Ice Sheet 14, 20–1, 31<br />

balance velocities calculated for grounded portion<br />

26<br />

DEMs for 16, 21, 22, 31–2<br />

InSAR-derived, north-east Greenland ice stream<br />

24<br />

ice divides 23–5, 25<br />

uncertainty in mass budget 13<br />

heat yield parameter 180, 181<br />

Helsinki University <strong>of</strong> Technology (HUT) snow<br />

emission model 51–2, 51, 52<br />

hydraulic model calibration and validation, practical<br />

consequences for flood envelope estimation<br />

and flood risk maps 80–1<br />

hydraulic modellers, predictive uncertainty a<br />

significant problem 80<br />

hydraulic models<br />

friction 86–7<br />

integration <strong>of</strong> spatial data with 92–100, 101<br />

inundation extent 82<br />

physically-based parameterization using LiDAR<br />

data 94, 95<br />

<strong>of</strong> reach scale flood inundation 81–2<br />

parameterization 86<br />

<strong>of</strong> friction 94<br />

trials against consistent inundation datasets 96<br />

use <strong>of</strong> LiDAR and airborne stereo-photogrammetry<br />

for automated broad-area mapping 86<br />

hydraulic resistance 79–80<br />

a lumped term 86<br />

hydrological cycle fluxes 246<br />

hydrological models, attempt to represent explicitly<br />

mass or energy transfers 10<br />

hydrology<br />

land surface modelling at large regional scales<br />

5–6<br />

spatial modelling in 9–12<br />

models constantly evolving 10<br />

physically-based models 9<br />

HYDROS (HYDROspheric States Mission) (NASA)<br />

66, 71, 73<br />

ice deformation 27<br />

ice divides 23–4<br />

for Greenland and Antarctica 24–5, 25<br />

ice flow models 11<br />

ice mass geometry 20<br />

ice sheet dynamics<br />

derived datasets 23–6<br />

fast-flow features<br />

ice sheet interior 26<br />

mechanisms 20, 27<br />

force-budget approach 30<br />

numerical models 19–21<br />

relationship between thickness and rheology 15,<br />

30<br />

<strong>the</strong>rmo-mechanical models, in situ rheology <strong>of</strong> <strong>the</strong><br />

ice 28, 30<br />

validation <strong>of</strong> models 26–30<br />

Greenland Ice Sheet, balance velocities cf.<br />

diagnostic velocities 26–9<br />

representation <strong>of</strong> <strong>the</strong>rmodynamics 28–9<br />

iso<strong>the</strong>rmal cases 27–8<br />

limitations in model resolution 29<br />

shallow ice approximation 29<br />

use <strong>of</strong> accurate surface DEMs for 30, 31<br />

ice sheet models 19–21<br />

key feedbacks 20<br />

ice sheet topography 4, 31<br />

derived from satellite radar altimetry 16–18<br />

from InSAR 18–19, 19, 22–3, 24<br />

from SRA 21–2<br />

parameterization in numerical modelling 14–15<br />

ice sheets<br />

impacts on <strong>the</strong> climate system 13–14<br />

surface pr<strong>of</strong>ile, dependence on ice rheology 30<br />

thickness <strong>of</strong> 15<br />

iceberg fluxes 25–6

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