1 Spatial Modelling of the Terrestrial Environment - Georeferencial
1 Spatial Modelling of the Terrestrial Environment - Georeferencial
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