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Guide to Hydrological Practices, 6th edition, Volume I - Hydrology.nl

Guide to Hydrological Practices, 6th edition, Volume I - Hydrology.nl

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I.2-24<br />

GUIDE TO HYDROLOGICAL PRACTICES<br />

Optimize operations<br />

Operational procedures account for a significant<br />

portion of the cost of data collection. This includes<br />

the types of instrument, frequency of station visits<br />

and structure of field trips. The minimum-cost<br />

operational procedures should be adopted.<br />

Budget<br />

Based on the identified network and operational<br />

procedures, the cost of the operation of the network<br />

can be established. If this is within the budget, the<br />

next step can be followed. If not, either additional<br />

funding must be obtained or the objectives and/or<br />

priorities need <strong>to</strong> be examined <strong>to</strong> determine where<br />

costs may be reduced. The process adopted should<br />

allow the designer <strong>to</strong> express the impact of insufficient<br />

funding in terms of not meeting objectives or<br />

reduced information and net impacts.<br />

Implementation<br />

The redesigned network needs <strong>to</strong> be implemented<br />

in a planned manner. This will include both shortand<br />

long-term planning horizons.<br />

Review<br />

Since a number of the above components are<br />

variable in time, a review can be required at the<br />

instigation of any particular component – for<br />

example, changes in users or uses, or changes in the<br />

budget. To be ready <strong>to</strong> meet such changes, a<br />

continuous review process is essential.<br />

2.4.2 Density of stations for a network<br />

The concept of network density is intended <strong>to</strong> serve<br />

as a general guideline if specific guidance is lacking.<br />

As such, the design densities must be adjusted <strong>to</strong><br />

reflect actual socio-economic and physio-climatic<br />

conditions. Computer-based mathematical analysis<br />

techniques should also be applied, where data are<br />

available, <strong>to</strong> optimize the network density required<br />

<strong>to</strong> satisfy specific needs.<br />

As stated in 2.4.1.3.1, the minimum network is one<br />

that will avoid serious deficiencies in developing<br />

and managing water resources on a scale commensurate<br />

with the overall level of economic<br />

development and environmental needs of the<br />

country. It should be developed as rapidly as possible,<br />

incorporating existing stations, as appropriate.<br />

In other words, such a network will provide the<br />

framework for expansion <strong>to</strong> meet the information<br />

needs of specific water uses.<br />

In the following sections, minimum densities of<br />

various types of hydrological stations are<br />

recommended for different climatic and<br />

geographic zones. These recommendations are<br />

based on the 1991 review of Members’ responses<br />

regarding the WMO basic network assessment<br />

project (WMO/TD-No. 671) and are presented in<br />

Table I.2.6. However, these recommended network<br />

densities are being revisited through a study<br />

undertaken by the Commission for <strong>Hydrology</strong> and<br />

the revised recommended densities will be placed<br />

on the Website as part of the electronic version of<br />

the <strong>Guide</strong>.<br />

It is impossible <strong>to</strong> define a sufficient number of<br />

zones <strong>to</strong> represent the complete variety of hydrological<br />

conditions. The simplest and most precise<br />

criterion for the classification of zones would be on<br />

the basis of the areal and seasonal variation of rainfall.<br />

Each country could present a good map of<br />

annual precipitation and a minimum network<br />

could be developed from this. However, this would<br />

Table I.2.6. Recommended minimum densities of stations (area in km 2 per station)<br />

Physiographic<br />

unit<br />

Precipitation Evaporation Streamflow Sediments Water quality<br />

Non-recording Recording<br />

Coastal 900 9000 50 000 2 750 18 300 55 000<br />

Mountains 250 2500 50 000 1 000 6 700 20 000<br />

Interior plains 575 5750 5 000 1 875 12 500 37 500<br />

Hilly/undulating 575 5750 50 000 1 875 12 500 47 500<br />

Small islands 25 250 50 000 300 2 000 6 000<br />

Urban areas – 10–20 – – – –<br />

Polar/arid 10000 100000 100 000 20 000 200 000 200 000

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