3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS,...

55
3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila http://cetemps.aquila.infn.it Marco Verdecchia CHyM: an operational distributed hydrological model using different data sources 3° ICTP Workshop on “The Theory and Use of Regional Climate Models” May 29 – June 9 2006

Transcript of 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS,...

Page 1: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CETEMPS, Physics Department, University of L‘Aquila

http://cetemps.aquila.infn.it

Marco Verdecchia

CHyM: an operational distributed hydrological model

using different data sources

3° ICTP Workshop on “The Theory and Use of

Regional Climate Models”May 29 – June 9 2006

Page 2: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Developed by:

Since 2002

•It runs in any geographical domain with any resolution•It runs in any (?) unix platforms•It does not use any licensed software•Different kind of rain data are assimilated

Page 3: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Two reasons for NOT using CHYM:

• NOT easy to use (CHyM is a NSE2USE Model)

• Documentation is not (yet) available

CHyM: an operational distributed hydrological model

using different data sources

Page 4: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Outline• Description of the model • Algorithms Generating streamflow network Building prec. fields with diff. data• Physical processes• Applications

CHyM: an operational distributed hydrological model

using different data sources

Page 5: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Why to develop a new Hydrological Model?

•It has been thought for operational purposes

•It is a good “exercise”

Page 6: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Step 1: generating streamflow network from DEM

DEM matrix for the selected domain and resolution is generated

Flow direction matrix is computed

Validation

“Pits” and singularities are corrected

Page 7: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

DEM is available with a resolution of 300 m

For each cell the slope is computed as:

Runoff direction

Max slope

Page 8: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Drainage network test

Page 9: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Drainage network test

Page 10: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

A Cellular Automata definitionA Cellular Automata definition

A cellular automaton is a A cellular automaton is a discrete dynamical discrete dynamical systemsystem Space, time and states of the system are discrete Space, time and states of the system are discrete quantitiesquantities

Each point in a regular spatial lattice, called a cell, Each point in a regular spatial lattice, called a cell, can have anyone of a finite number of statescan have anyone of a finite number of states

The state of the cells in the lattice are updated The state of the cells in the lattice are updated according to a according to a local rulelocal rule

All cells on the lattice are All cells on the lattice are updated synchronouslyupdated synchronously

Page 11: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

A Cellular Automata A Cellular Automata applicationapplication

Life rules by Chris G. Langton

The status of each CA can be ON or OFF

If more than 3 CA in the neighborhood are ON CA became OFF

If less than 2 CA in the neighborhood are ON, CA became OFF

Otherwise CA became ON

Page 12: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CA for CHyM applicationsCA for CHyM applications

CHyM grid is considered an aggregate of cellular CHyM grid is considered an aggregate of cellular automataautomata

The status of a cell corresponds to the value of aThe status of a cell corresponds to the value of a

The state of the cells in the lattice is updated The state of the cells in the lattice is updated according to followingaccording to following rule rule

All cells on the lattice are updated synchronouslyAll cells on the lattice are updated synchronously

Update ends when flow scheme is OKUpdate ends when flow scheme is OK

8

)(j

ijjii hhhh

CHyM matrix (DEM)CHyM matrix (DEM)

Page 13: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Recipe for DEM pit correction

•Smooth DEM using CA rules until FD can be obtained for all the cells

•Generate streamflow network using smoothed DEM

•Use “true” DEM and modify ONLY the cells draining toward an higher cell

Page 14: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Drainage network test

Page 15: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Page 16: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Page 17: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: DEM pit correction

Page 18: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: DEM pit correction

Page 19: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: DEM pit correction

Page 20: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Examples of Drainage Network Extraction

Page 21: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: the Rolling Stones Algorithm (RSA)

2. Each time that the stone goes through one cell for this cell a counter is incremented by 1

1. Starting from each cell a stone rolls up to the river‘s mouth

3. If a quantity A is associated to each stone where Ais equivalent to the surface where the stone was at the beginning, for each cell it can be computed theupstream drained surface

N

iiA

1

4. If a quantity R is associated to each stone where Ris equivalent to the precipitation where the stone was at the beginning, for each cell it can be computed theupstream drained precipitation

N

iiR

1

Page 22: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: the Rolling Stones Algorithm (RSA)

Page 23: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

MuseoArchive

MM5 analysis MM5 Forecast

Now

timeRadar Gauge data

Satellite estimations

Step 2: Building Precipitation Fields using different Data Sources

Page 24: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM rain data sources: Gauge measurements

Page 25: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM rain data sources: Radar estimates

Page 26: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

NERETIR

NEural RainfallEstimationfromTermalInfraRed

CHyM rain data sources: NERETIR

Page 27: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

MM5 Meteorological Model

CHyM rain data sources: MM5

Page 28: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Step 2: Building Precipitation Fields using different Data Sources

Module 1

Module 2

Module 3

Module n

•Define subdomain•Fill cells corresponding to rain gauges•Fill subdomain matrix – Cr. Formula•Smooth subdomain matrix using CA algorithm

Page 29: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CA for CHyM applicationsCA for CHyM applications

CHyM grid is considered an aggregate of cellular CHyM grid is considered an aggregate of cellular automataautomata The status of a cell corresponds to the value of a CHyM matrix The status of a cell corresponds to the value of a CHyM matrix

The state of the cells in the lattice is updated The state of the cells in the lattice is updated according to followingaccording to following rule rule

All cells on the lattice are updated synchronouslyAll cells on the lattice are updated synchronously

Update ends when flow scheme is OKUpdate ends when flow scheme is OK

8

)(j

ijjii hhhh

But cells corresponding to rain gauges or defined in a previous Module are not updated

Update ends when a stable state is reachedUpdate ends when a stable state is reached

(RAIN)(DEM)

Page 30: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Observed rain using Cressman

algorithm

+ smoothing usingCellular Automata

jj ij

iji R

ar

arR

22

22

1

1rij≤ a

Page 31: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

+ MUSEO module using Cressman

+ CA

Page 32: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9In sequence …

Page 33: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM Rain field sources: an example

Page 34: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Runoff EvapotraspirationInfiltrationRainfall

For each cell the simulated processes are:

Page 35: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Infiltration

Soil moisture storage

Deep percolation

Infiltration

Interflow

Surface Runoff

Page 36: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: Evapotraspiration

Thornthwaite Formula (Thornthwaite and Mather, 1995)

Page 37: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9CHyM: Runoff

Continuity equation

Momentum equation

cqx

Q

t

A

An

RSQ

3221

A= cross sectional area of the riverQ= flow rate of water dischargeqc= rain for length unit

S= slope

1/R= wetter perimeter

n= Manning‘s roughness coefficient

Page 38: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

AIA

R

N

ii

N

ii

1

1 Ri = rain

Ai = drained surface

AI= Alarm Index

CHyM: A first application

Page 39: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Page 40: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Soverato Floodsimulation

Page 41: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Val Canale floodsimulation

Page 42: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: simulation of Aug 22-23 2005 event

Flood alert mapping using MM5 and CHyM

Page 43: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: simulation of Aug 22-23 2005 event

Flood alert mapping using MM5 and CHyM

Page 44: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: simulation of Aug 22-23 2005 event

Page 45: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Landslides prediction using CHyM. (Very) Preliminary results

•Daily precipitation from 1958 to 2002

•Total drained rain in the last N days

•Landslides occur when TDR-N is greater than LT (N and LT values to optimized)

Page 46: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Page 47: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

Page 48: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Landslides prediction using CHyM. (Very) Preliminary results

Page 49: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Landslides prediction using CHyM. (Very) Preliminary results

Page 50: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Landslides prediction using CHyM. (Very) Preliminary results

Page 51: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

Landslides prediction using CHyM. (Very) Preliminary results

Page 52: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: hydrological effects due to Alpine Glaciers Melting

Page 53: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed hydrological model

using different data sources

For further information about the model and related literature please visit the URL:

http://cetemps.aquila.infn.it/chym/

Page 54: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9

CHyM: an operational distributed

hydrological model using different data sources

Page 55: 3° ICTP Workshop “The Theory and Use of Regional Climate Models” May 29 – June 9 CETEMPS, Physics Department, University of L‘Aquila .

3° I

CT

P W

orks

hop

The

The

ory

and

Use

of

Reg

ion

al C

limat

e M

odel

s”M

ay 2

9 –

Jun

e 9