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7. Toward a Global Hydrological Network


In section 4., the major applications requiring hydrological observations were identified. To meet these observation requirements, a capability must exist to evaluate requirements and to acquire, assemble and make available global data sets of hydrological observations. This capability should be able to deliver observations with the appropriate spatial resolution, observational frequency, timeliness, and quality. It is proposed that these roles be met by a Global Terrestrial Network for Hydrology, GTN-H. This network would complement other existing global terrestrial networks grouped under GT-Net (http://www.fao.org/GTOS/PAGES/Gtnet.htm), namely GTN-G for glaciers, GTN-P for permafrost, and GTN-E for ecosystem observations (see also section 2.3, 2.4).

The primary users of GTN-H products will include international conventions (Framework Convention on Climate Change, Convention on Biological Diversity, Convention to Combat Desertification); global observing systems; major water-related programmes and initiatives of the United Nations; the research community with focus on national to global scales; and regional and national agencies concerned with climate change impacts and sustainable development. As discussed in more detail below, the network would initially be formed through an association of existing data acquisition networks, data assembly facilities, and product generation centres; new capabilities would be added as and where required and feasible.

7.1 Functions

GTN-H is envisioned to have the following functions:

In general, GTN-H activities will concentrate on hydrological data and products, including data acquisition and assembly; product generation, distribution and archiving; etc. However, GTN-H must also be linked with, and responsive to, a broader framework, both thematically and organisationally. For example, from a climate perspective the main objective is to observe regional and local changes in hydrological variables that respond to or force climate, directly or indirectly, and to understand the processes by which these variations occur, rather than documenting climate change detection per se.

Figure 3 illustrates some of the GTN-H functions and feedback loops. An important distinction needs to be made on the basis of timeliness of data delivery. Real-time hydrological data are needed continually for numerical weather prediction, for some aspects of seasonal climate forecasting, as well as for assessment of hydrologic conditions when anticipating hydrologic hazards such as flooding. These measurements can be assimilated directly into the models, thus requiring no further assembly or generation of products. The data can now be made available primarily through GTS, a system established and operated to support the World Weather Watch Programme of WMO, NWP and related applications. However, it may be feasible to also use the Internet for data transmission such as currently done nationally by the USGS; this aspect would require careful analysis of the implications for global distribution. As Figure 3 indicates, products requiring assembly, screening and processing of the original observations are produced in delayed time, with the length of delay varying depending on the nature of the product as well as the data handling capabilities.

In general, GTN-H is concerned with the terrestrial portion of the global water cycle, that is, the movement of water on, above and below the earth's surface. Therefore, it must interface with other aspects of the earth system: energy fluxes and biogeochemical cycles, notably the global carbon cycle and its terrestrial component; terrestrial sediment flux processes; the oceanic, atmospheric, and cryospheric parts of the global water cycle; and the earth's climate. For the same reasons, GTN-H evolution needs to include consultation and collaboration with programs and agencies that are concerned with these aspects of the earth system.

Figure 3. The General Context and Data Functions of GTN-H

7.2 Attributes

GTN-H is envisioned to have the following major characteristics:

It is suggested that the spatial context of individual sites in GTN-H be established using global site - specific data sets with designated hydrologic connectivity between sites as well as global gridded data sets, with the grid cell size chosen in relation to the requirement as well as to the data type(s) under consideration. Normally, the various grid sizes would be nested, giving flexibility in scaling and data handling. The catchment topology (stream networks, watershed boundaries, topography, land cover and land use distribution) can also be readily accommodated through co-registered overlays. These various GTN-H attributes can be readily linked once placed in a geographic context, and existing information processing tools (e.g., geographic information system software) can be used to achieve efficient data utilisation. Initial steps in this direction have been taken by GRDC and UNH (see also section 6.1 and 6.12). The various levels of observation intensity at individual sites can be accommodated through the tier concept of the Global Hierarchical Observation Strategy (GHOST; GCOS/GTOS, 1997).

7.3 GTN-H Components

It is envisioned that GTN-H will consist of several components, which are necessary to carry out the functions identified in section 7.1 and illustrated in Figure 3. Figure 4 considers these from the perspective of the existing networks and proposed participating agencies. A number of the hydrological variables of interest are presently being collected (section 6.), and a subset is being made available. Most of the data collection takes place at the national level, executed and funded by national hydrological or meteorological agencies. To various degrees, these data are presently assembled by international centres to generate global or regional products (section 6.). Figure 4 indicates that these centres are at various stages of evolution. For some variables (discharge, precipitation, snow water equivalent, isotopic composition of precipitation, BGC fluxes into oceans, vapour pressure) such centres and associated data access mechanisms exist; in these cases, some products are being generated and others are feasible during the initial phase of GTN-H establishment. For other variables (evapotranspiration), data collection is underway and centres for data use exist, however data access is not well developed. For the remaining variables (surface water storage fluxes, ground water fluxes, soil moisture, water use), the main problems are inadequate data collection, difficult access to relevant information, lack of data handling centres, or a combination of these. Figure 4 also shows the centres that are sufficiently developed and active to become effective GTN-H contributors from the outset. These issues are addressed further in the discussion on GTN-H implementation plan (section 7.5) and recommendations (section 8.).

To ensure success of the GTN-H, an end-to-end approach needs to be adopted for its planning and implementation. The term "end-to-end" management of data and information describes a process rather than a sequence of actions. In particular, it implies the establishment of a feedback loop between the providers of data and information and the user of the information (Figure 3).

Figure 4. Proposed Initial Configuration of GTN-H

The specific arrangements for data flow are likely to differ based on the type of data, the characteristics and capabilities of contributing sites and networks, and the timeliness requirements. As an example, Figure 5 shows the potential use of the Internet for handling the access to runoff data and the derived products.

State - of - the - art information systems and communication technology are at the heart of the proposed GTN-H. Information will also flow from/to GOSIC, INFOCLIMA, INFOHYDRO and INFOTERRA. In the development of the GTN-H it is essential to establish linkages with existing data centres. This is particularly important where additional data and variables are the subject of related programmes and projects such as water quality and isotopes in hydrology.

Figure 5. A Scenario for GTN-H Data and Product Delivery via Internet

7.4 Hydrological Observation Panel for Climate

Three global observing systems have been established in the 1990s to enable systematic, long-term observation and assessment of the earth system in general, and the role of climate in particular: the Global Climate Observing System (GCOS, 1995; http://www.wmo.ch), the Global Ocean Observing System (GOOS; http://ioc.unesco.org/goos/goostoc.htm); and the Global Terrestrial Observing System (GTOS, 1998; http://www.fao.org/gtos). These are in addition to the World Weather Watch (http://www.wmo.ch) and other WMO programs which have been in existence for many years and which provide the relevant atmospheric observations. Each of these observing systems encompasses space and in situ observations, and each is organised to maximise the efficiency and effectiveness of making the observations for global as well as regional applications.

The overall direction for the development of each global observing system is provided by a steering committee. In turn the scientific input to the steering committee as well as some implementation activities are the mandate of scientific panels established as part of the programs. Since from the scientific as well as organisational perspectives many of the observation issues are very broad, the implementation of the global observing systems must be approached through close collaboration with other activities in the observation and scientific communities. This is dealt with by ensuring broad representation of observation and research agencies in the steering committees, and by co-sponsorship of the science panels. In general, these panels are sponsored jointly by two or more international programs. The terms of reference for the panels are defined by the panel's co-sponsors, and the panels report to all the sponsoring organisations. The co-sponsorship helps ensure that the various programs are co-ordinated at the scientific and technical levels, and that the advice provided to the steering committees has been formulated in the broad context of related activities. In this way, the science panels are responsible to the major international programs that are relevant to the panels' work. In the terrestrial domain, two science panels have been established for the Global Terrestrial Observing System so far: the Terrestrial Observation Panel for Climate (TOPC) in 1995 and the Global Observation of Forest Cover (GOFC) Panel in 2000.

Since hydrology issues concern mainly the terrestrial environment, TOPC has been the panel responsible for these on behalf of GCOS and GTOS. Its activities included an initial analysis of the observation issues and identification of critical variables (GCOS, 1997), definition of satellite observation requirements (TOPC, 1998), and others (GTOS, 2000). However, there are other important hydrological issues beyond TOPC terms of reference that are relevant to GTOS' five themes, especially sustainable availability of water resources and pollution/toxicity (GTOS, 1998). These have been dealt with to some extent by TOPC (TOPC, 1999) but only at a general level. Application areas discussed at this workshop (section 3., 4.) have confirmed the importance of the non-climate issues in the terrestrial hydrological domain, and have highlighted the urgent need for more focused attention to this area.

An important task of the science panels is to contribute to the initial implementation of the observing systems. Thus, TOPC has led the establishment of global in situ observing networks, initially built by co-ordinating activities of existing networks and engaging these in systematic global observation. Three such networks have been established so far (TOPC, 1999) that focus on ecology <http://www.ilternet.edu/>, glaciers <http://www.geo.unizh.ch/wgms/>, and permafrost <http://sts.gsc.nrcan.gc.ca/permafrost/gtn-p.htm>. Similarly, GOFC has developed regional networks as part of its implementation (Figure 6). This expert meeting developed the framework for a similar network in hydrology but it also identified a number of critical issues that require scientific guidance and initiative. Previous experience from the global observing systems demonstrates that scientific advice is a critical element of success for the observation networks and of the products the networks generate.

Based on the above considerations, it is proposed that in addition to GTN-H, a Hydrological Observation Panel for Climate (HOPC) be established as a new science co-ordinating panel with an advisory function. Its terms of reference might be patterned TOPC (Annex IV.), with due considerations to hydrology-specific science and organisational aspects as well as the present situation, programs and concerns. In particular, they need to recognise that hydrological issues are complex scientifically, administratively, and politically. Figure 6 shows GTN-H as a network that receives organisational, administrative and scientific guidance primarily from HOPC, although its activities are also important to some aspects of the mandate of TOPC and other similar groups. To be successful, HOPC will need to receive guidance from the sponsoring agencies in developing recommendations and proposed actions that are practical, lead to progress, and meet the needs and expectations of the sponsors.

The composition of HOPC will be crucial for the successful implementation GTN-H. In addition to the representation of the sponsoring agencies, panel members should provide linkages to sponsoring agencies, the agencies participating in GTN-H, the scientific community, and to clients/product users. Establishing these cross-linkages will be a key mechanism for enabling GTN-H to work efficiently and effectively. GTOS, GCOS, WMO and its constituent programs, ICSU, and IHP/UNESCO are among the desirable sponsors. Major GTN-H participants should also be represented (Figure 4).

Figure 6. The Proposed Organisational Relationships Involving GTN-H

7.5 Initial Implementation

To advance the implementation of systematic global hydrological observation, the following activities are proposed by the participants:

In developing GTN-H the design of the metadata base as well as database implementation, operation and maintenance should be components of the strategic plan. A metadata base will also be required to handle information about the data that will be used to assist in interpretation and analysis.

7.6 Proposed Products

Table 2 describes potential GTN-H products that were identified by meeting participants as important to a variety of clients, with several being feasible within the initial GTN-H period.

Table 2. Proposed GTN-H Products for the Initial Period

Product name

Content

Use

Spatial resolution

Temporal resolution

Time- liness

Contact

Discharge

gridded runoff fields

Water balance computations

1o x 1o

Monthly (ongoing)

DT (delayed time)

GRDC (W. Fröhlich)

Discharge

Point data

Weather forecasting (model validation)

N/A

Daily (ongoing)

NRT (near-real time)

GRDC (W. Fröhlich)

Soil moisture

Gridded (preferably)

Weather forecasting (assimilation in models)

TBD

Daily (ongoing)

NRT

CEOP (J. Leese)

Discharge

Regional totals

Global water cycle analysis

by region

Monthly

DT

GRDC (W. Fröhlich)

Discharge

Point data

Regional water cycle analysis

For CEOP regions

Daily and monthly > (CEOP period)

DT

GRDC (W. Fröhlich)

BGC flux into oceans

By major watershed

Global BGC cycles analysis

By watershed

Daily to monthly (ongoing)

DT

GEMS Water (A. Fraser)

Isotope composition

d18O, d2H, 3H

Various

By station

Weekly to monthly (ongoing)

DT

IAEA (M. Gröning)

Hydrographic separation

Discharge as % of inputs

Regional water cycle analysis

By watershed

Weekly to monthly (ongoing)

DT

IAEA (M. Gröning)

Isotope composition

d18O, d2H

Global BGC cycles analysis

By station

Weekly to monthly (ongoing)

DT

IAEA (M. Gröning)

Hydrographic separation

Discharge as % of inputs

Global BGC cycles analysis

By watershed

Weekly to monthly (ongoing)

DT

IAEA (M. Gröning)

Precipitation

Solid and liquid

Regional water cycle analysis

For CEOP regions

Daily (CEOP period)

DT

GPCC (B. Rudolf)

Precipitation

Solid and liquid separately

Regional water cycle analysis

1dx1d globally; 0.5o x 0.5o regionally

Daily and monthly (global ongoing, regional for limited periods)

DT

GPCC (B. Rudolf)

Snow water equivalent

Gridded

Various

TBD

TBD

DT

NOAA

Ground water fluxes

Aquifer withdrawal rates

Various

By aquifer

TBD

DT

TBD

Water use

Differentiated consumptive use

Various

Point or polygon

Monthly, ongoing

DT

GRDC (W. Fröhlich) University of Kassel, P. Döll

Water use

Gridded consumptive use

Various

0.5o x 0.5o

Monthly

DT

University of Kassel, P. Döll

Surface storage Flux

Volume changes in lakes and reservoirs

Water cycle analysis

Polygon

Monthly or seasonal (ongoing)

DT

TBD

Precipitation, evapotrans-piration, Other

Point data

Real time data for assimilation in models

Point

Daily

RT

TBD

7.7 Resources Required and Available

As a basis of the day-to-day operation of GTN-H, the participants felt that the collaborating institutions and data centres should cover operating expenses from their existing budgets. However, additional resources will be required to fund co-ordination activities of GTH-N and to assist partners who may have not sufficient resources to participate fully in the GTN-H activities. This is especially important in developing countries whose collaboration must be sought.

The following incremental cost items were identified:

Sources of funding were discussed in detail and the group agreed on the following list of sources for potential funding extra-budgetary activities of GTN-H:

Taking into consideration operating guidelines of the existing centres, GTN-H is expected to operate within the framework of major resolutions of the constituent bodies of the sponsoring UN agencies, including Resolutions 25 and 40 of WMO which concern the exchange of hydrological information. To ensure sustainability of GTN-H, international funding for programme development and operations must be an integral part of the strategy. Without financial commitment for resources at a level necessary for sustained activity by partner agencies, the GTN-H will not be successful. The participants agreed to investigate funding opportunities and encouraged collaborating centres and agencies to pro-actively seek additional funding to support GTN-H activities.

7.8 Potential Contributions

Workshop participants identified potential contributions to GTN-H that may be feasible from within existing resources. The delivery of these contributions needs to be confirmed through discussions with management of the network operators and agencies participating in GTN-H:

7.9 Follow-up Actions

Based on the above discussions and the issues raised, participants identified a number of follow-up activities that are needed to pursue the development of the GTN-H. These include:


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