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s n i s a b r e v i r n a c i r f A n i e c a p s m o r f t h g u o r d d n a s d o o l f g n i r o t i n o M

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d n a t n e s e r P , t s a P e h t f o w e i v e R t r o h S A

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s e u g a e ll o c C T I y l n i a m , r e h t o m o r f s e d il s l a r e v e s g n i s U

s n i s a b r e v i r n a c i r f A n i e c a p s m o r f t h g u o r d d n a s d o o l f g n i r o t i n o M

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What is waiting for us in this presentation…?

Definitely neither a history nor an EO lesson!

Although we start with the first Earth Observation satellites What is optical RS?

First applications: colour composites

Statistical approaches: image classification

Physical EO examples: evaporation and water quality The future: GEOSS

What WM problems are dealt with in Africa: with the example of the TIGER Capacity Building Facility

A WM project with EO application in Iran

So, this is to show seriously with exmaples that EO is fun!

17-28 September 2012 NFP refresher course UDSM 2

(3)

3

When was the first satellite launched?

4 October 1957 – 4 January 1958 Sputnik 1 Russian

Sent radio signals continuously and its orbit was monitored (geophysical measurements)

Source: http://en.wikipedia.org/wiki/Satellite

(4)

4

When was the first imaging earth observation satellite launched?

1 April 1960, TIROS-1 700-750 km altitude Television images

Operational for 78 days

Source: http://en.wikipedia.org/wiki/TIROS-1

(5)

5

Development in forty years…

TIROS-1 1960

Source: www.leos.le.ac.uk/mipas/main.html

† Died in May 2012

(6)

6

The first RS image

Source:

http://en.wikipedia.org/wiki/File:TIROS-

1-Earth.png

(7)

7

Why remote sensing?

Synoptic overview

Additional information compared to field measurements/maps

Measurement of hydrology-related parameters: e.g. water-covered areas, temperature, water depth (in limited cases), soil moisture, evapotranspiration.

The best PR material for RS in daily use: Google Earth

(8)

8

Spectral characteristics of optical RS sensors

Energy sources

Atmospheric transmittance

Common RS systems

© Lillesand & Kiefer, 1994

(9)

9

First applications in the seventies: interpretation of RGB colour composites

(Virtually Hawaii 1999)

(10)

By the way: One of the first RGB composite images

17-28 September 2012 NFP refresher course UDSM 10

Mohammed Alim Khan (1880–1944), Emir of

Bukhara

1911 by Sergei M.

Prokudin-

Gorskii using three

exposures with red, green, and blue filters.

Source:

Wikipedia

(11)

11

Colour composites (Landsat TM)

Natural CC False CC

(http://academic.emporia.edu/aberjame/remote/landsat/landsat.htm)

(12)

12

Special Landsat TM CC

Lake Van, Turkey

Special CC (127)

Andes, Peru

Special CC (235)

(http://academic.emporia.edu/aberjame/remote/landsat/landsat.htm)

(13)

13

Special LandsatTM CC

Special CC (375)

Infrared CC (457)

Paris, France White Sands, Mexico

(http://academic.emporia.edu/aberjame/remote/landsat/landsat.htm)

(14)

1150 km 14

Pushbroom Imager ( 5 cameras) Total swath width: 1150 Km Full Resolution: 300 m

Reduced resolution: 1200 m

VIS-NIR Spectrometer within spectral range: 390 to 1040 Nanometers 15 bands electronically programmable (in width and position)

A space-borne imaging spectrometer: MERIS on ENVISAT (ESA)

Source of slide: C. Stewart, ESA

(15)

25

Wind

L a te n t H ea t (P h a se c h a n g e)

Example of physical RS: surface energy balance (starting from the nineties)

Z. Su, 2005

(16)

15

In this MERIS image the contrast can clearly be seen between the desert areas of Senegal in the north to the vegetated coastal plains of Guinea- Bissau, The Gambia and Southern Senegal (shown in red on the image).

Acquistion: 24-Feb-2004

Example of MERIS images

The green colour of the sea around the islands of the Buagos Archipelago is caused by sediment being swept out to sea from the river

Source of slide: C. Stewart, ESA

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16

Objective: Converting image data into thematic information

Statistical methods – from the seventies

(18)

17

Image space

Multi-band Image

(19)

18

One-dimensional feature space

Input layer

Distinction between classes

No distinction between classes

(20)

19

Multi-dimensional feature space

Feature vectors

(21)

20

Series of two-dimensional feature spaces

(22)

21

Problems in image classification

Constraints of pixel based image classification

it results in spectral classes

each pixel is assigned to one class only

Spectral bands - Spectral classes - Land cover - Land use Land cover

Grass Training samples

Spectral classes

Meadow Land use

Sport

(23)

22

Problems in image classification

Mixed Pixels

Terrain Image

(24)

23

Image classification result

Classified Ikonos image April 2000

Enschede

Applications ????

(25)

Physical process: Light interaction with materials on Earth

17-28 September 2012 NFP refresher course UDSM 24

R.S. Instrument Sun

Clouds

transmitted radiation

Scattered radiation*

Atmospheric absorption

Earth

Reflection processes Emission processes Thermal emission

Atmospheric emission Reflected

radiation scattered

radiation**

* selective scatter (blueish optical images)

** non-selective scatter (white clouds)

Atmosphere Atmospheric

interactions

(26)

25

Wind

L a te n t H ea t (P h a se c h a n g e)

Example of physical RS: surface energy balance (starting from the nineties)

Z. Su, 2005

(27)

26

SEBS Core Modules

Boundary Layer Similarity Theory

Roughness for Heat Transfer Surface Energy Balance Index

Meteorological Data Boundary Layer Variables

Remote Sensing Data VIS

NIR TIR

Input Output

Evaporative Fraction Turbulence Heat Fluxes

Actual Evaporation

Z. Su, 2005

SEBS: the Surface Energy

Balance System

(28)

Spatial Distribution of Annual Evaporation over the Urumqi River Basin

27

(29)

Interactions with the surface

© Lillesand & Kiefer, 1994

Principle of conservation of energy

The relative amount of each energy ( R,A,T ) changes with

28 Tiger Capacity Building Facility II.

Advanced Optical RS – 14-20. September 2010.

(30)

29

Physical RS: Water quality

Specific inherent optical properties

(SIOP) are absorption (a*) and scattering (b*) per unit of mass.

Source: [6]

0 5 10 15 20 25

400 500 600 700 800 900

Wavelength, nm

a * c d o m ,a _ w ( m ^ -1 )

0 0.005 0.01 0.015 0.02 0.025 0.03

a * c h l (m 2 / m g ), a * ts m (m 2 / g ) a_w

a_dom a_tsm a_chl

0 0.05 0.1 0.15 0.2 0.25 0.3

400 500 600 700 800 900

Wavelength, nm b * ts m (m ^ 2 / g ) , b * c h l (m ^ 2 / m g )

0 0.0005 0.001 0.0015 0.002 0.0025 0.003 0.0035

b b _ w (m ^ -1 )

b_tsm bb_chl b_w

Mean specific absorption (left) and backscattering (right) coefficients

(31)

30

Example of physical RS with imaging spectrometry: water quality mapping

Spatial distribution of chlorophyll a (left) and suspended matter (right) for lake ‘Tegeler See’ on 23 April 1995

retrieved by a look-up table approach from CASI images.

Source: Dekker et al, 2001

(32)

31

Tandem mode for radar interferometry

(33)

32

Elevation changes due to earthquake along a fault

(California, USA)

(34)

33

Overflowing

Overtopping

Piping

Sliding inner slope

Plastic horizontal sliding

Nipping ice

Dike monitoring with In-SAR

BLUE Below Sea level

17000 km of water barriers:

3565 km primary water barriers (big rivers, sea, IJsselmeer, Markermeer),

>14000 km regional water barriers

On the potential of PS-InSAR for

monitoring dikes in the Netherlands

Courtesy R. Hansen Delft Institute of Earth

Observation and Space Systems

(35)

34

Landsat background, with PSI- dike results of 9 frames

superposed (1992-2005)

On the potential of PS-InSAR for monitoring dikes in the Netherlands

Courtesy of Ramon Hansen Delft Institute of Earth Observation and Space Systems

~90% of dikes monitored !!

(36)

GEOSS

35

Global Earth Observation System of Systems:

This emerging public infrastructure is interconnecting a diverse and growing array of instruments and systems for monitoring and forecasting changes in the global environment.

This “system of systems” supports policymakers, resource

managers, science researchers and many other experts and

decision-makers. (source: http://earthobservations.org/)

(37)

17-28 September 2012 NFP refresher course UDSM 36

TIGER Capacity Building Facility

EO in Africa: Capacity building for research

TIGER Capacity Building Facility

(38)

TIGER Projects

Carry out research

Receive data from the TIGER programme Receive support and supervision from TCBF:

Supervisor

Tailored capacity building plan Promotion of results

37 The TIGER

Initiative

(39)

38

(40)

Number of projects which include the keyword

Keywords

1 Carbon sequestration; Drought;

Groundwater; Nutrient surplus;

Rainfall; Real-time monitoring;

Sediment transport; Spatial database;

Vulnerability

2 Algal bloom / aquatic plants; Change detection;

Forest cover / biomass; Irrigation / water demand;

Operational monitoring; Risk mapping 3 Land use / land cover change;

Modelling

4 Flood monitoring / water body mapping;

Decision support system, planning

5 Water balance

6 Climate change

7 Water quality

8 Water management

10 Water resources

39 The TIGER

Initiative

(41)

Test areas

40 The TIGER

Initiative

(42)

Types of data used in the projects

Data type Number of projects

High resolution optical (1-30 m) 9

Medium resolution optical (30-300 m) 20

Coarse resolution optical (>300 m) 13

High resolution SAR (1-30 m) 9

Medium resolution SAR (30-300 m) 10

Coarse resolution SAR (>300 m) 0

41 The TIGER

Initiative

(43)

Example: Mara wetland, Tanzania

42 The TIGER

Initiative

(44)

TCBF home page http://www.itc.nl/tiger/default.asp

43

(45)

44

A project example: Lake Uromiyeh

Hypersaline lake

(46)

45

Problem: water allocation between agriculture and the ecosystem

1272 1273 1274 1275 1276 1277 1278 1279

Jan-69 Jan-79 Jan-89 Jan-99

m a .m .s .l .

Lake level

Water stage - volume curve of Lake Uromiyeh

0 5 10 15 20 25 30

1270 1272 1274 1276 1278

T h o u s a n d s

Water stage [m a.m.s.l]

V o lu m e [ m 3 ]

0 1 2 3 4 5 6

T h o u s a n d s L a k e s u rf a c e [ k m 2 ]

Lake volume Lake surface

(47)

46

Groundwater over-exploitation

Tassoj plain groundwater hydograph (94-2002))

1307 1309 1311 1313 1315 1317 1319 1321 1323

94- 95 95- 96 96- 97 97- 98 98- 99 99- 2000 2000- 2001 2001- 2002

Month/Years

G ro u n d w a te r le v e ls (m )

(48)

47

(49)

48

How can we meet the needs of the society?

Integrated landscape management

Integrated land resources management Integrated water resources management

=>

Complex approach, multidisciplinarity

(50)

49

Modelling approach to IWRM in Uromiyeh

ILWIS GIS

HYMOS Hydrological

Data Base

&

Modeling System

RIBASIM

Dmand Analysis Allocation Analysis Definite

Impact Assessment

&

Scenario Analysis Agriculture

Urban Industrial

Environmental

River Basin Simulation

Water Allocation to

Different Users

(51)

50

Input to the system: precipitation

precipitation 1993-94 precipitation 1999-2000

(52)

51

Losses from the system using SEBAL

actual evapotranspiration 1993-94 actual evapotranspiration 1999-

2000

(53)

52

Modelled sub-watershed: Gadar Chai

Gadarchai river

basin wetlands

(54)

53

!"!# $%&'( ' )*+'& , -.!/ 0#!12# 3 #

Agriculture grav irr naghadeh chaparabad sys.

Area=5000ha Agriculture grav irr

oshnaviyeh chaparabad sys. Area=11000ha

Agriculture grav irr hassanlu sys.

Area=4000ha

Gadar chi river

Groundwater total of naghadeh&

oshnaviyeh Orumiyeh

Lake

Yadgarl wetland Supply water

for indu&munici

Hassanlu dam

Dorgesangii wetland

Soldoziw etland Gelaxchi-osh basin

area=103km2 q=1.49m3/sec

Godarchi-payghaleh basin area=255km2 q=9.07m3/sec

Kanirash - chaparabad area=243km2 q=1.04m3/sec

Shaykhanrod-dorood basin area=62.2km2 q=1.36

Balighchi-balighchy basin area=230km2 q=.82m3/sec

Biram-moham..

Area=202.5km2 q=.63m3/sec

Conceptual model of Ghadar Chai

(55)

54

Long-term calibration of flow

0 3 6 9 12 15 18 21 24 27 30

19 68 19 69

19 70 19 71

19 72 19 73

19 74 19 75

19 76 19 77

19 78 19 79

19 80 19 81

19 82 19 83

19 84 19 85

19 86 19 87

19 88 19 89

19 90 19 91

19 92 19 93

19 94 19 95

19 96 19 97

19 98 19 99

20 00 20 01

Year Y ea rl y d is ch a rg e (m 3 /s ec )

Measurement

Calculated

(56)

55

Future developments

Agriculture grav irr naghadeh chaparabad sys. Area=9628ha

Agriculture pre irr naghadeh chaparabad sys. Area=2307ha Agriculture pre irr oshnaviyeh

chaparabad sys. Area=6926ha Agriculture grav irr oshnaviyeh

chaparabad sys. Area=15837ha Agriculture pre irr

payghaleh chaparabad sys.

Area=1445ha Agriculture grav irr

hassanlu sys.

Area=8473ha

Gadar chi river

Groundwater total of naghadeh&

oshnaviyeh

Agriculture pre irr hassanlu sys.

Area=5523ha

Orumiyeh Lake

Yadgarl wetland Supply water

for indu&munici

Hassanlu dam

Chaparabad dam

Dorgesangiiwe tland

Soldoziwet land Gelaxchi-osh basin

area=103km2 q=1.49m3/sec

Godarchi-payghaleh basin area=255km2 q=9.07m3/sec

Kanirash - chaparabad area=243km2 q=1.04m3/sec

Shaykhanrod-dorood basin area=62.2km2

q=1.36 Fish pond

Balighchi-balighchy basin area=230km2 q=.82m3/sec

Biram-moham..

Area=202.5km2

q=.63m3/sec

(57)

56

Scenarios

Agriculture without efficiency increase

Priority 1: domestic and industrial supply

Priority 2: agriculture and fishponds with present efficiency Priority 3: wetlands with present demand + streamflow

Agriculture with efficiency increase

P1: domestic and industrial supply

P2: agriculture and fishponds with increased efficiency P3: wetlands with increased demand + streamflow

Environment without efficiency increase

P1: domestic and industrial supply

P2: wetlands with present demand + streamflow P3: agriculture and fishponds with present efficiency

Environment with efficiency increase

P1: domestic and industrial supply

P2: wetlands with increased demand + streamflow

P3: agriculture and fishponds with increased efficiency

(58)

57

Conceptual model of the Uromiyeh Basin

Agriculture grav irr naghadeh chaparabad sys.

Area=5000ha Agriculture grav irr

oshnaviyeh chaparabad sys. Area=11000ha

Agriculture grav irr hassanlu sys.

Area=4000ha

Gadar chi river Groundwater total of naghadeh&

oshnaviyeh

Orumiyeh Lake

Yadgarl wetland Supply water

for indu&munici

Hassanlu dam

Dorgesangii wetland

Soldoziw etland Gelaxchi-osh basin

area=103km2 q=1.49m3/sec

Godarchi-payghaleh basin area=255km2 q=9.07m3/sec

Kanirash - chaparabad area=243km2 q=1.04m3/sec

Shaykhanrod-dorood basin area=62.2km2 q=1.36

Balighchi-balighchy basin area=230km2 q=.82m3/sec

Biram-moham.. Area=202.5km2 q=.63m3/sec Shahr chi River

Mirabad st.

No: 1 q= 5.24 m3/sec V= 165 m.c.m

Inter Basin No: 4

Inter Basin No: 5 Ups Band Agr.

A= 385 ha demand=3.31 m.c.m

Urban and Indusrrial Demand=

m.c.m

Inter Basin No: 3

Inter Basin No : 6 Down Band Agr.

A=2730 ha Demand=23.45 m.c.m

Mid Kashtiban Agr.

A=5130 ha Demand=44.07 m.c.m

Ups Kashtiban Agr.

A=1655 ha Demand=14.22 m.c.m

Down Kashtiban Agr.

A=1100 ha Demand=9.45 m.c.m Ground water Reservoir V=60 m.c.m

Baranduz chi river

Mahabad chi river Tasoj to sofian chi

Sofi chi river

Simineh rood river

Zarineh rood river Nazlo chi river

Zola chi river

Groundwater total of Baranduz chi Supply water for

indu&munici total Baranduzchi basin Agriculture Left up balanush area= ha

Agriculture left down balanush area= ha

Agriculture right up balanush area=

ha Enter dischage dam site locate (baranduz)

Agriculture right down balanush area= ha enter basin dize - babarood Balanush hyd. Station

Agriculture mahabad left river Area=5672.5 ha

kanibrazan wetland

Ghooy baba ali wetland

Agriculture mahabad right river Area=5916ha

Mahabad dam

Supply water for indu&munici total mahabad basin

Bitas hyd. station kooter hyd.station Dehbokr hyd.

station

Varsho chi river Chekan chi -Chekan Hyd. station Sofi chi riverSofichi - Tazehkand Hyd. station

Alavian dam

Supply water for indu&munici Maragheh city

Supply water for indu&munici Bonab city

Irrigation area right bank river sofichi area= 9365 ha Irrigation area left bank river sofichi area= 2835 ha

Groundwater total of Sofichi chi

From zarineh rood

Agricultural Demand Dashband from sw(pumping)

Agricultural Demand Dashband from sw(gravity)

Agricultural Demand Bookan from sw(pumping)

Agricultural Demand Bookan from sw(gravity)

Agricultural Demand Sharikand from sw(pumping)

Agricultural Demand Sharikand from sw(gravity)

Enter discharge tosystem

Pole anian hyd.

St.

Karimabad hyd.st.

Safakhanehhyd.st.

Mahmud abadHyd. St. Dare panbeh dan hyd. St.

Inter basin

Zarinehrood dam Agricultural

Demand Shahindezh

Groundwater Shahindezh Supply water for indu&munici Shahindezh

Chobloche hyd. St.

chalekh maz Hyd. St.

Agricultural Demand Mianduab Supply water for indu&munici Mianduab city

GroundwaterMi anduab Shirin kandy hyd. St. Inter basin

Mardugh hyd. St.

Supply water for indu&munici Tabriz city

Inter basin

Inter basin

Saransar= 133.6 MCM

Sarab GW SarabAgiculture

Area= 5000 ha

Mehraban= 55.68 MCM

Bostan Abad= 63.10 MCM BostanabadAgiculture

Area= 11466 ha Mehraban Agiculture

Area= 17000 ha

Mehraban &

Bostanabad Domestic demand

Kordkandi reservoir

Mehraban& Bostanabad GW

Pajchi= 26.95 MCM

Nahand chi= 42.94MCM

Nahand reservoir

Tabriz Domestic demand

Tabriz GW

Saeedabadchi= 11.07 MCM

Sardrood=9.305 MCM Lighvanchi=21.5 MCM Gomnabchi=34.11 MCM Senikh chi= 27.26MCM

Senikh chi (Pardil)=35.09 MCM

TabrizAgiculture Area=

34000 ha Vanyar reservoir

(under construction)

Zarrinehrood Line Aji Chi

Rozeh chi river Rozeh chi river

calhor Hyd.

station Nazlo chi river tepic hyd. Station.

Agricultural Demand for Nazlochi basin Ground water

Reservoir Nazlochi basin Supply water for

indu&munici total Nazlo chi basin Zolachi river Dam Site (Zola) Derik river Nazarabad Hyd.

station

Ground water Reservoir Nazlochi basin Supply water for

indu&munici total Nazlo chi basin

Salmas city Agricultural Demand

for Nazlochi basin Salmas plain

(59)

58

Major conclusions of the project

The recent water use is already more than the environmentally tolerable.

Further development without efficiency improvement is killing Lake Uromiyeh.

Even the planned efficiency improvement is not enough for balancing the

population pressure (increasing agricultural production) and the need for

energy production.

(60)

59

Thank you!

Hivatkozások

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