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natural hazards, and usually lack the resources to invest in

adequate infrastructure. Poverty limits choice, and forces

people to take risks, such as living on land vulnerable to

flooding or landslip. Many humanitarian and environmental

disasters are directly related to weather and water. Some occur

on very short timescales, such as hurricanes and flash floods.

Others, such as droughts and food shortages, can be stretched

over a period of months, or even several years. Even when

not directly involved in a hazard, weather often complicates

attempted relief and rescue operations. In the short term,

disaster warning systems can prevent much loss of life and

livelihood by alerting people to particular threats. Climate

change will alter the incidence of natural disasters, as well as

having impacts on the sustainability of environments and

livelihoods over the coming decades. Because of this, quality

information is vital to prepare people to adapt their liveli-

hoods.

The primary source of funding for NMHS is for the provi-

sion of the public weather service. Thus, validation of this

service has become increasingly important in order to justify

government funding. In developing countries, as a broad gener-

alization, NMHS get very little funding from private-sector

work, even where they are able to exploit commercial oppor-

tunities. Commercial aviation weather services, for those

NMHS which provide them, are a very important part of the

justification argument, since international civil aviation pays

the national authorities in hard currency. Unfortunately, in

many countries this does not translate directly into funds for

the NMHS.

Developing country NMHS have great difficulty with afford-

ing the equipment for observing the environment. This is

particularly the case with the consumables for upper-air

measurement. Each radio-sonde observation costs approxi-

mately USD200. With developments in numerical weather

prediction and satellite capability, as well as the data gath-

ered by Aircraft Meteorological Data Relay (AMDAR)

equipment on civil airline flights, there is no longer scien-

tific justification for upper air observations, as beneficial to

local forecasting. The exceptions are for low-level aviation

forecasting and applications such as tracing pollutants and

disease vectors. Increasingly, the primary requirements for a

network of high-quality upper air observations are to provide

a long-term record for monitoring global climate, and to

provide the baseline calibration for satellite instruments.

Surface observations generally have lower costs. Though the

capital cost of equipment may be significant, the unit cost for

each observation will be made up mainly from staff and

communication expenses. There is also a much stronger argu-

ment for the utility of surface observations in providing local

and national benefit. Surface observations are also commu-

nicated and used globally; under international agreements

through WMO, observations from the Global Climate

Observing System and other networks are freely available

through NMHS and global data centres.

It can be seen that environmental observation data and meta-

data has high costs, but the value of the observation lies in the

use made of it, and not in the observation itself. Hence it is

unrealistic to argue that any individual user of the observation

should pay a particular proportion of the cost. Even if charges

are levied on users for the cost of observations, it is very diffi-

cult to make these equitable, and the result is likely to be that

potential services will be rendered uneconomic. In contrast, it

Photo: Instituto Nacional de Meteorologia, Spain

Commissioning a solar photometer at Tamanrasset in Southern Algeria

with support from Spain to monitor aerosols and dust in air masses

over the Sahara desert, especially for early warning of dust clouds

is generally in the interest of NMHS to increase the number

and range of users of their data in order to strengthen their

case for adequate government funding for the public weather

service. Therefore charges for the use of data should reflect the

value added by the information and services derived from said

data.

It is instructive to consider these data using the concept of

‘Global Public Good’

3

where ‘good’ means a thing or condition

(in this case data and the metadata needed to interpret it) but

makes no assumptions about the costs, benefits or valuation

of the good; ‘global’ means spanning all divides and borders;

‘public’ refers to the general population, civil society organi-

zations and corporate citizens; the ‘global public’ includes states

and international organizations. These observations therefore

meet the economists’ definition of ‘public good’ as having both

non-excludable and non-rival benefits, as well as being non-

exclusive. It is worth emphasising the huge potential current

and future benefits of these observations in providing a clima-

tological record during a period of rapid change, in supporting

current forecasting on periods from immediate response to

seasons, and in providing the baseline and future verification

as the climate changes. However, only some of these benefits

will accrue in the countries where the observations are taken,

particularly in the developing countries. Remote islands are

especially important for global observations, and many of these

are in Small Island Developing States. It is likely that the major-

ity of economic benefits of “global public good” observations

will accrue in developed countries, despite the developing

countries suffering most from the social impacts of extreme

events and climate change.

This analysis shows why it is difficult to persuade develop-

ment aid partners, whose interests are primarily to enhance

free trade and economic growth, achieve sustainable develop-

ment, promote good governance and democracy and increase

safety and security, to be interested in funding observations,

particularly of the upper air. For funding by NMHS of devel-

oped countries, including through the WMO VCP, it is