Appropriate scales for hydro-climatological variables in the Red River basin

Martijn J. Booij, H.M. Tran

Research output: Chapter in Book/Report/Conference proceedingConference contributionAcademicpeer-review

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Abstract

Decision support systems (DSSs) in water management should preferably consist of appropriate models, which are complex enough to represent important processes at a balanced level, but not unnecessarily refined, taking into account research objectives, data availability and uncertainties. This idea is illustrated by applying a methodology for the determination of appropriate scales to the hydrological part of a DSS. The variability of a relevant variable at the point scale, the discharge at the outlet, is used to determine the appropriate temporal scale. The appropriate spatial scale for precipitation is then determined at this appropriate temporal scale. Results indicate an appropriate temporal scale varying between 12 h for middle-sized upstream areas to 48 h for the complete river basin, accepting an aggregation error of 10%. The appropriate spatial scale for precipitation for the complete river basin is about 80 km. The appropriate scales found are important for the hydrological model set-up and may indicate the requirements for downscaling from climate model to hydrological model scale for climate impact assessments.
Original languageUndefined
Title of host publicationRegional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295
EditorsThorsten Wagener, Stewart Franks, Hoshin V. Gupta, Eva Boegh, Luis Bastidas, Carlos Nobre, Carlos de Oliveira Galvao
PublisherIAHS Press
Pages325-332
Number of pages356
ISBN (Print)9781901502084
Publication statusPublished - 3 Apr 2005

Publication series

NameIAHS publication
PublisherIAHS Press
Number295
ISSN (Print)0144-7815

Keywords

  • Precipitation
  • Variance reduction function
  • Temporal scales
  • Discharge
  • Red River basin
  • Appropriateness
  • Spatial scales
  • Decision-support system

Cite this

Booij, M. J., & Tran, H. M. (2005). Appropriate scales for hydro-climatological variables in the Red River basin. In T. Wagener, S. Franks, H. V. Gupta, E. Boegh, L. Bastidas, C. Nobre, & C. de Oliveira Galvao (Eds.), Regional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295 (pp. 325-332). (IAHS publication; No. 295). IAHS Press.
Booij, Martijn J. ; Tran, H.M. / Appropriate scales for hydro-climatological variables in the Red River basin. Regional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295. editor / Thorsten Wagener ; Stewart Franks ; Hoshin V. Gupta ; Eva Boegh ; Luis Bastidas ; Carlos Nobre ; Carlos de Oliveira Galvao. IAHS Press, 2005. pp. 325-332 (IAHS publication; 295).
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keywords = "Precipitation, Variance reduction function, Temporal scales, Discharge, Red River basin, Appropriateness, Spatial scales, Decision-support system",
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Booij, MJ & Tran, HM 2005, Appropriate scales for hydro-climatological variables in the Red River basin. in T Wagener, S Franks, HV Gupta, E Boegh, L Bastidas, C Nobre & C de Oliveira Galvao (eds), Regional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295. IAHS publication, no. 295, IAHS Press, pp. 325-332.

Appropriate scales for hydro-climatological variables in the Red River basin. / Booij, Martijn J.; Tran, H.M.

Regional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295. ed. / Thorsten Wagener; Stewart Franks; Hoshin V. Gupta; Eva Boegh; Luis Bastidas; Carlos Nobre; Carlos de Oliveira Galvao. IAHS Press, 2005. p. 325-332 (IAHS publication; No. 295).

Research output: Chapter in Book/Report/Conference proceedingConference contributionAcademicpeer-review

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T1 - Appropriate scales for hydro-climatological variables in the Red River basin

AU - Booij, Martijn J.

AU - Tran, H.M.

PY - 2005/4/3

Y1 - 2005/4/3

N2 - Decision support systems (DSSs) in water management should preferably consist of appropriate models, which are complex enough to represent important processes at a balanced level, but not unnecessarily refined, taking into account research objectives, data availability and uncertainties. This idea is illustrated by applying a methodology for the determination of appropriate scales to the hydrological part of a DSS. The variability of a relevant variable at the point scale, the discharge at the outlet, is used to determine the appropriate temporal scale. The appropriate spatial scale for precipitation is then determined at this appropriate temporal scale. Results indicate an appropriate temporal scale varying between 12 h for middle-sized upstream areas to 48 h for the complete river basin, accepting an aggregation error of 10%. The appropriate spatial scale for precipitation for the complete river basin is about 80 km. The appropriate scales found are important for the hydrological model set-up and may indicate the requirements for downscaling from climate model to hydrological model scale for climate impact assessments.

AB - Decision support systems (DSSs) in water management should preferably consist of appropriate models, which are complex enough to represent important processes at a balanced level, but not unnecessarily refined, taking into account research objectives, data availability and uncertainties. This idea is illustrated by applying a methodology for the determination of appropriate scales to the hydrological part of a DSS. The variability of a relevant variable at the point scale, the discharge at the outlet, is used to determine the appropriate temporal scale. The appropriate spatial scale for precipitation is then determined at this appropriate temporal scale. Results indicate an appropriate temporal scale varying between 12 h for middle-sized upstream areas to 48 h for the complete river basin, accepting an aggregation error of 10%. The appropriate spatial scale for precipitation for the complete river basin is about 80 km. The appropriate scales found are important for the hydrological model set-up and may indicate the requirements for downscaling from climate model to hydrological model scale for climate impact assessments.

KW - Precipitation

KW - Variance reduction function

KW - Temporal scales

KW - Discharge

KW - Red River basin

KW - Appropriateness

KW - Spatial scales

KW - Decision-support system

M3 - Conference contribution

SN - 9781901502084

T3 - IAHS publication

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BT - Regional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295

A2 - Wagener, Thorsten

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A2 - Gupta, Hoshin V.

A2 - Boegh, Eva

A2 - Bastidas, Luis

A2 - Nobre, Carlos

A2 - de Oliveira Galvao, Carlos

PB - IAHS Press

ER -

Booij MJ, Tran HM. Appropriate scales for hydro-climatological variables in the Red River basin. In Wagener T, Franks S, Gupta HV, Boegh E, Bastidas L, Nobre C, de Oliveira Galvao C, editors, Regional hydrological impacts of climate variability and change - Impact assessment and decision making. Symposium HS06 at IAHS 2005, 3-9 April 2005, Foz do Iguaçu, Brazil. IAHS publication 295. IAHS Press. 2005. p. 325-332. (IAHS publication; 295).