Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-018-4166-7 |
Climate downscaling over South America for 1971-2000: application in SMAP rainfall-runoff model for Grande River Basin | |
Roque da Silva, Felipe das Neves1,2; Drummond Alves, Jose Luis2; Cataldi, Marcio3 | |
2019 | |
发表期刊 | CLIMATE DYNAMICS
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ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2019 |
卷号 | 52页码:681-696 |
文章类型 | Article |
语种 | 英语 |
国家 | Brazil |
英文摘要 | This paper aims to validate inflow simulations concerning the present-day climate at agua Vermelha Hydroelectric Plant (AVHPlocated on the Grande River Basin) based on the Soil Moisture Accounting Procedure (SMAP) hydrological model. In order to provide rainfall data to the SMAP model, the RegCM regional climate model was also used working with boundary conditions from the MIROC model. Initially, present-day climate simulation performed by RegCM model was analyzed. It was found that, in terms of rainfall, the model was able to simulate the main patterns observed over South America. A bias correction technique was also used and it was essential to reduce mistakes related to rainfall simulation. Comparison between rainfall simulations from RegCM and MIROC showed improvements when the dynamical downscaling was performed. Then, SMAP, a rainfall-runoff hydrological model, was used to simulate inflows at agua Vermelha Hydroelectric Plant. After calibration with observed rainfall, SMAP simulations were evaluated in two different periods from the one used in calibration. During calibration, SMAP captures the inflow variability observed at AVHP. During validation periods, the hydrological model obtained better results and statistics with observed rainfall. However, in spite of some discrepancies, the use of simulated rainfall without bias correction captured the interannual flow variability. However, the use of bias removal in the simulated rainfall performed by RegCM brought significant improvements to the simulation of natural inflows performed by SMAP. Not only the curve of simulated inflow became more similar to the observed inflow, but also the statistics improved their values. Improvements were also noticed in the inflow simulation when the rainfall was provided by the regional climate model compared to the global model. In general, results obtained so far prove that there was an added value in rainfall when regional climate model was compared to global climate model and that data from regional models must be bias-corrected so as to improve their results. |
英文关键词 | Hydrometeorological modeling Regional climate model Global climate model Hydrological model SMAP RegCM Bias correction |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000460619200039 |
WOS关键词 | REGIONAL CLIMATE ; CHANGE IMPACT ; BIAS CORRECTION ; PRECIPITATION ; SIMULATION ; SENSITIVITY ; CONVECTION ; EUROPE ; CLIMATOLOGIES ; CIRCULATION |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/35496 |
专题 | 气候变化 |
作者单位 | 1.Fed Ctr Technol Educ CEFET RJ, Coordenadoria Meteorol, Av Maracana 229,Bloco A, BR-20271110 Rio De Janeiro, RJ, Brazil; 2.Fed Univ Rio De Janeiro UFRJ, Ctr Tecnol, Bloco 1,Sala 214 Av Athos Silveira Ramos, BR-21941909 Rio De Janeiro, RJ, Brazil; 3.Fluminense Fed Univ UFF, Rua Passo Patria,156 Bloco D, BR-24210240 Niteroi, RJ, Brazil |
推荐引用方式 GB/T 7714 | Roque da Silva, Felipe das Neves,Drummond Alves, Jose Luis,Cataldi, Marcio. Climate downscaling over South America for 1971-2000: application in SMAP rainfall-runoff model for Grande River Basin[J]. CLIMATE DYNAMICS,2019,52:681-696. |
APA | Roque da Silva, Felipe das Neves,Drummond Alves, Jose Luis,&Cataldi, Marcio.(2019).Climate downscaling over South America for 1971-2000: application in SMAP rainfall-runoff model for Grande River Basin.CLIMATE DYNAMICS,52,681-696. |
MLA | Roque da Silva, Felipe das Neves,et al."Climate downscaling over South America for 1971-2000: application in SMAP rainfall-runoff model for Grande River Basin".CLIMATE DYNAMICS 52(2019):681-696. |
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