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Using response function concepts to model groundwater ... - WHYCOS

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Drought measurement


Overview<br />

• Definitions of drought<br />

• Raro<strong>to</strong>nga case study<br />

• Practical exercise – Excel example<br />

– Rainfall depreciation method (weighted sum)<br />

– Decile method


Reactions <strong>to</strong> the 1997-98 El Nino<br />

• Water supply reliability severely tested<br />

– Kiribati - impact on <strong>groundwater</strong> lens<br />

– Marshall Is - interest in desalination<br />

– Fiji Is - Suva water supply, Drought Emergency<br />

– Cook Islands - need for demand management<br />

• Questions<br />

– How long is the current drought going <strong>to</strong> last<br />

– How severe is it What can be done<br />

– How frequently can droughts be expected


Drought as a Natural Hazard<br />

• Loss of life<br />

• health problems<br />

• increased risk of fire<br />

• deterioration of water quality<br />

• loss of agricultural production<br />

• increased demand for water<br />

• salt water intrusion


Drought Definitions<br />

• Partial or <strong>to</strong>tal absence of rainfall or<br />

irregular distribution during a period in<br />

which precipitation should occur<br />

• prolonged or abnormal moisture deficiency<br />

• “a worrisome lack of rain”<br />

• Meteorological, Agricultural, Hydrological,<br />

Socioeconomic


The Climate / Drought Linkage<br />

Climatic State<br />

Precipitation Anomaly<br />

Water Resources Anomaly<br />

(low stream flows, <strong>groundwater</strong> and soil moisture<br />

levels)<br />

Drought Effects<br />

(loss of production, health problems, etc.)


Measuring Drought<br />

• Climate data based<br />

– Palmer Drought Index (PDI)<br />

– Standardized Precipitation Index (SPI)<br />

– Decile (percentile ranking)<br />

– Rainfall depreciation<br />

• Effects based<br />

– Remote sensing<br />

– Socioeconomic survey of impacts


Reducing Drought Consequences<br />

• Coping e.g.<br />

– leak detection & control<br />

– water conservation campaigns<br />

– emergency water supplies<br />

• Adaptation e.g.<br />

– changes in farming patterns<br />

– drought <strong>to</strong>lerant species<br />

– irrigation<br />

– drought management plans


Case study


Raro<strong>to</strong>nga, Cook Islands<br />

• Reticulated water supply dependent on<br />

several small catchments<br />

• No effective s<strong>to</strong>rage<br />

• Limited control on water use from<br />

reticulated supply<br />

• Need for demand management and leak<br />

control


Raro<strong>to</strong>nga Water Supply - Overview<br />

• 12 Water intakes sited within small<br />

catcment areas<br />

• 4 Underground horizontal water galleries<br />

• 120km pipeline network<br />

• Limited s<strong>to</strong>rage<br />

• Untapped <strong>groundwater</strong>


Raro<strong>to</strong>nga water supply<br />

Very low water flow<br />

in stream/high flow losses<br />

in pipeline network


Impact of recent drought on<br />

Raro<strong>to</strong>nga water supply<br />

Instream filterbeds dry


Impact of drought on Raro<strong>to</strong>nga<br />

water supply<br />

Stream flow diverted<br />

in<strong>to</strong> intake by-pass<br />

line


Raro<strong>to</strong>nga Water Supply<br />

May 98 July 98


Raro<strong>to</strong>nga Water Supply<br />

Water Supply Management requires<br />

methods for:<br />

– Early warning of drought events<br />

– Prediction of severity and duration<br />

– Prediction of future drought events<br />

– Drought severity/duration/frequency<br />

To manage drought we need <strong>to</strong> measure it


Weighted Sum Index<br />

Uses a time window with increasing weight<br />

given <strong>to</strong> most recent rain (a measure of<br />

catchment memory)<br />

Weighted Sum Index<br />

2000<br />

1800<br />

1600<br />

1400<br />

1200<br />

1000<br />

800<br />

600<br />

400<br />

200<br />

0<br />

30 35 40 45 50 55 60 65 70 75 80 85 90 95<br />

Year


Drought Forecast<br />

Long term rainfall forecast allows a forecast<br />

of drought persistence<br />

Weighted Sum Index<br />

1400<br />

1200<br />

1000<br />

800<br />

600<br />

400<br />

Monthly Rainfall (mm)<br />

300<br />

250<br />

200<br />

150<br />

100<br />

50<br />

0<br />

97.03 97.08 98.01 98.06 98.11<br />

Date


Raro<strong>to</strong>nga Management Options<br />

• Public information <strong>to</strong> increase public and<br />

political awareness<br />

• Control of irrigation watering from the<br />

reticulated supply<br />

• Bans on specified classes of water use<br />

during severe or extreme droughts


Information Needs<br />

• need for information <strong>to</strong> allow <strong>response</strong> <strong>to</strong> a<br />

particular drought<br />

• need for information on viable strategies for<br />

coping with drought<br />

• need information on the nature of the<br />

drought hazard -<br />

severity/duration/frequency


Practical exercise<br />

• Use Suva or Nadi monthly time series data<br />

<strong>to</strong> calculate drought indices:<br />

– Deciles<br />

• PERCENTRANK <strong>function</strong><br />

– Rainfall depreciation method<br />

• Index = 0.9*R 0 +0.8*R 0 +0.7*R 0 +0.6*R 0 etc.

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