TOPLATS 지표해석모형 기반의 고해상도 수문성분 평가
Evaluation of High-Resolution Hydrologic Components Based on TOPLATS Land Surface Model
0
조회
0
다운로드
3
인용
0
참고문헌
키워드
초록
High spatio-temporal resolution hydrologic components can give important information to monitor natural disaster. The objective of this study is to create high spatial-temporal resolution gridded hydrologic components using TOPLATS distributed land surface model and evaluate their accuracy. For this, Andong dam basin is selected as study area and TOPLATS model is constructed to create hourly simulated values in every 1 × 1km2 cell size. The observed inflow at Andong dam and soil moisture at Andong AWS site are collected to directly evaluate the simulated one. RMSEs of monthly simulated flow for calibration (2003~2006) and verification (2007~2009) periods show 36.87 mm and 32.41 mm, respectively. The hourly simulated soil moisture in the cell located Andong observation site for 2009 is well fitted with observed one at −50 cm. From this results, the cell based hydrologic components using TOPLATS distributed land surface model show to reasonably represent the real hydrologic condition in the field. Therefore the model driven hydrologic information can be used to analyze local water balance and monitor natural disaster caused by the severe weather.
Abstract
High spatio-temporal resolution hydrologic components can give important information to monitor natural disaster. The objective of this study is to create high spatial-temporal resolution gridded hydrologic components using TOPLATS distributed land surface model and evaluate their accuracy. For this, Andong dam basin is selected as study area and TOPLATS model is constructed to create hourly simulated values in every 1 × 1km2 cell size. The observed inflow at Andong dam and soil moisture at Andong AWS site are collected to directly evaluate the simulated one. RMSEs of monthly simulated flow for calibration (2003~2006) and verification (2007~2009) periods show 36.87 mm and 32.41 mm, respectively. The hourly simulated soil moisture in the cell located Andong observation site for 2009 is well fitted with observed one at −50 cm. From this results, the cell based hydrologic components using TOPLATS distributed land surface model show to reasonably represent the real hydrologic condition in the field. Therefore the model driven hydrologic information can be used to analyze local water balance and monitor natural disaster caused by the severe weather.
참고문헌 (24)
- 강전호, "지면경계조건이 UM을 이용한 동아시아 여름철 단기예보에 미치는 영향", 대기, 21(4), pp.415~427 (2011), 한국기상학회
- 김형진, "대기 대순환 모형과 지면모형의 접합에 관하여", 한국기상학회지, 41(6), pp.1137~1149 (2005), 한국기상학회
- 하경자, "다층 지면과정 모형접합에 대한 AGCM의 민감도 실험", 한국기상학회지, 34(4), pp.630~642 (1998)
- Betts, A., "Assessment of the land surface and boundary layer models in two operational versions of the NCEP Eta model using FIFE data", Mon. Weather Rev, 125, pp.2896~2916 (1997)
- Beven, K., "Runoff production and flood frequency in catchments of order n: an alternative approach, In Scale Problems in Hydrology", pp.107~131 (1986), Reidel
- Beven, K., "A physically based, variable contributing area model of basin hydrology", Hydrological Sciences Bulletin, 24(1), pp.43~69 (1979)
- A generalized streamflow simulation system: Conceptual models for digital computers, "Burnash, R. J. C.", Joint Fed.-State River Forecast Cent, ~, pp.Technical Report (1973)
- Chen, F., "Impact of atmospheric surface layer parameterizations in the new land-surface scheme of the NCEP mesoscale Eta model", Boundary Layer Meteorology, 85, pp.391~421 (1997)
- Crow, W. T., "Upscaling of field-scale soil moisture measurements using distributed land surface modeling", Advances in Water Resour, 28, pp.1~14 (2005)
- The non-hydrostatic limited-area model LM(Lokal-Modell) of the DWD, "Doms, G.", Deutscher Wetterdienst, ~, pp.Technical Report, 180. (1999)
- Ek, M. B., "Implementation of Noah land surface model advances in the National Centers for Environmental Prediction operational mesoscale Eta model", J. Geophys. Res, 108(D22), pp.8851~ (2003)
- Famiglietti, J. S., "Application of multiscale water and energy balance models on a tallgrass prairie", Water Resour. Res., 30(11), pp.3061~3078 (1994)
- Koster, R., "The components of a SVAT scheme and their effects on a GCM's hydrological cycle", Advances in Water Resour., 17, pp.61~78 (1994)
- Koster, R., "Variance and predictability of precipitation at seasonal-to-interannual timescales", J. Hydrometeorology, 1, pp.26~46 (2000)
- Liang, X., "A simple hydrologically based model of landsurface water and energy fluxes for GCMs", J. GeophysRes, 99, pp.415~428 (1994)
- Yoon-Jin Lim, "A Land Data Assimilation System Using the MODIS-Derived Land Data and Its Application to Numerical Weather Prediction in East Asia", 한국기상학회지, 48(1), pp.83~95 (2012), 한국기상학회
- Milly, P. C. D., "An event based simulation model of moisture and energy fluxes at a bare soil surface", Water Resour. Res, 22, pp.1680~1692 (1986)
- Monteith, J. L., "Evaporation and environment, in: Sympos. The state and movement of water in living organism", pp.205~234 (1965), Cambridge Univ Press
- Peters-Lidard, C. D., "A reexamination of modeled and measured soil moisture spatial variability and its implications for land surface modeling", Advances in Water Resour, 24, pp.1069~1083 (2001)
- Rawls, W. J, "Use of soil texture, bulk density, and the slope of the water retention curve to predict saturated hydraulic conductivity", Trans. ASAE, 41(4), pp.983~988 (1998)
- Rawls, W. J., "Estimation of soil water properties", Trans. ASAE, 25(5), pp.1316~1320 (1982)
- Seuffert, G., "The influence of hydrologic modeling on the predicted local weather: two-way coupling of a mesoscale weather prediction model and a land surface hydrologic model", J. Hydrometeorology, 3, pp.505~523 (2002)
- Sivapalan, M., "On hydrologic similarity. 2. A scaled model of storm turnoff production", Water Resour. Res., 23, pp.2266~2278 (1987)
- Wood, E. F., "Hydrological modeling of continental-scale basins", Annu. Rev. Earth Planet. Sci, 25, pp.279~300 (1997)
