abstract soria

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Sensitivity analysis in the evaluation of the effects of land use change in discharge rate *FREDDY SORIA 1 , SO KAZAMA 2 , MASAKI SAWAMOTO 1 1. Gradu ate School of Engine ering, Civi l Engineeri ng Department, T ohok u Universit y , 6-6- 06, Aobayama, Aob a-ku, Sendai, 980-8579, Japan 2. Gradu ate School of Environme ntal Studies, T ohok u University , 6-6-06, Ao bayama , Aoba- ku, Sendai, 980-8579, Japan *E-mail address of corresponding author: [email protected] Abstract Change of conditions and spatial distribution of land use and vegetation is an element that contributes to climatic evolution, since it has an important effect on the variables of the hyd rol ogi cal cyc le, hen ce in wat ersh eds res pon se. The pot ent ial and sop his tic atio n of hyd rol ogi cal mod els has gre atl y inc reas ed, and nowadays dis tri but ed mod els are wid ely availa ble tools for the analysi s of the spatial variabi lity of hydr ologi cal processes. Lately the interest has moved beyond, from the evaluation of changes in the present (i.e. the next 10 years), to the evaluation of the impacts of climate change in the near future (i.e. 10 to 30 years from the present) and longer-term basis (i.e. few more decades beyond). Climate models have  born from such interest, and as in the case of distributed hydrological models, they have evolv ed and impro ved their capacity to describ e the dynamics of events, their resolu tion has increased, and has also grown the number of variables and processes predicted. The data generated by the climate models is used in this manuscript as the input in a particular scheme of a distributed hydrological model, and the contribution of this paper is to present the importance of sensitivity analysis of the model components and model output (i.e. discharge rate) to different scenarios of land use change due to predicted climatic conditions. To illustrate the ideas, a distributed hydrological model is applied in Caine River basin, Ce nt ral Bolivia. Future condit ions are taken from data pr oduced by the Model for  Interdisciplinary Research on Climate (MIROC 3.2), a coupled general circulation model with 100km spatial resolution, and 3h, 6h to daily resolution for climatic variables. Under such conditions, variance based analysis is used for the evaluation of model components and watersh ed response sensitivity to land use and vegetat ion change. The scenarios driven after the conditions established by MIROC’ predictions are compared against observed data, and are found somehow overestimated, therefore the impact of land use and vegetation change on wat ersh ed resp onse obt ained her e can be assu med as for the wor st case scenar io. The sensitivity analysis showed that the impact of land use and vegetation change scenarios could

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Page 1: Abstract SORIA

7/27/2019 Abstract SORIA

http://slidepdf.com/reader/full/abstract-soria 1/2

Sensitivity analysis in the evaluation of the effects of land use change in

discharge rate

*FREDDY SORIA

1

, SO KAZAMA

2

, MASAKI SAWAMOTO

1

1. Graduate School of Engineering, Civil Engineering Department, Tohoku University, 6-6-

06, Aobayama, Aoba-ku, Sendai, 980-8579, Japan

2. Graduate School of Environmental Studies, Tohoku University, 6-6-06, Aobayama, Aoba-

ku, Sendai, 980-8579, Japan

*E-mail address of corresponding author: [email protected]

Abstract

Change of conditions and spatial distribution of land use and vegetation is an element that

contributes to climatic evolution, since it has an important effect on the variables of the

hydrological cycle, hence in watersheds response. The potential and sophistication of 

hydrological models has greatly increased, and nowadays distributed models are widely

available tools for the analysis of the spatial variability of hydrological processes. Lately the

interest has moved beyond, from the evaluation of changes in the present (i.e. the next 10

years), to the evaluation of the impacts of climate change in the near future (i.e. 10 to 30 years

from the present) and longer-term basis (i.e. few more decades beyond). Climate models have

 born from such interest, and as in the case of distributed hydrological models, they have

evolved and improved their capacity to describe the dynamics of events, their resolution has

increased, and has also grown the number of variables and processes predicted. The data

generated by the climate models is used in this manuscript as the input in a particular scheme

of a distributed hydrological model, and the contribution of this paper is to present the

importance of sensitivity analysis of the model components and model output (i.e. discharge

rate) to different scenarios of land use change due to predicted climatic conditions.

To illustrate the ideas, a distributed hydrological model is applied in Caine River basin,Central Bolivia. Future conditions are taken from data produced by the Model for 

Interdisciplinary Research on Climate (MIROC 3.2), a coupled general circulation model with

100km spatial resolution, and 3h, 6h to daily resolution for climatic variables. Under such

conditions, variance based analysis is used for the evaluation of model components and

watershed response sensitivity to land use and vegetation change. The scenarios driven after 

the conditions established by MIROC’ predictions are compared against observed data, and

are found somehow overestimated, therefore the impact of land use and vegetation change on

watershed response obtained here can be assumed as for the worst case scenario. The

sensitivity analysis showed that the impact of land use and vegetation change scenarios could

Page 2: Abstract SORIA

7/27/2019 Abstract SORIA

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 be more critical in locations with convergent and divergent topography, perhaps due to higher 

impact of erosive processes.

Keyword:Climate change, distributed modeling, variance based sensitivity analysis.