Location: Coastal Plain Soil, Water and Plant Conservation Research
Title: Quantifying the probabilistic divergences related to time-space scales for inferences in water resource managementAuthor
Sohoulande, Clement | |
Stone, Kenneth | |
SINGH, VIJAY - Texas A&M University |
Submitted to: Agricultural Water Management
Publication Type: Peer Reviewed Journal Publication Acceptance Date: 3/1/2019 Publication Date: 5/20/2019 Citation: Sohoulande Djebou, D.C., Stone, K.C., Singh, V.P. 2019. Quantifying the probabilistic divergences related to time-space scales for inferences in water resource management. Agricultural Water Management. 217:282-291. https://doi.org/10.1016/j.agwat.2019.03.004. DOI: https://doi.org/10.1016/j.agwat.2019.03.004 Interpretive Summary: In water resources modeling the frequency of measurement and the spatial distribution of data can have a considerable impact on the results and their interpretation. However, studies focusing on time-pace scales issues are few. In this research, a methodology is developed to enable an understanding of the impact induced by the scales on water resources variables. The study addresses eight variables: streamflow, groundwater level, precipitation, temperature, soil moisture, solar radiation, wind speed, and relative humidity. For each variable, 10-year (2001 to 2010) daily time series data were obtained from weather and hydrologic stations selected across the State of Oklahoma. The daily values of the selected variables were rescaled at weekly, monthly, bimonthly, and trimonthly scales. The rescaled data were then analyzed using a probability theory and tested for divergence from the original daily data. Results show meaningful divergences from the original daily data. These divergences are a consequence of time-space scales variations. However, the sensitivity of the variables to the scales were different. For instance, air temperature was less sensitive to time-space scales while wind speed, soil moisture, and precipitation were highly sensitive. Correlation analysis showed that the correlations tend to gradually increase with the increase in scale, but the relation varied depending on the variables involved. The methodology was tested via a case study where data obtained from a location outside of the study region were used to address the scales effect on the Normalized Difference Vegetation Index’s response to precipitation and soil moisture. It was concluded that understanding the divergences associated with scales was critical for interpreting results in water resources studies. Technical Abstract: Studies focusing on time-space scaling issues have not yet established guidelines for choosing a time-space scale for water resources management. This study attempts to develop a methodology to understand the deviations induced by the scaling framework on water resource variables. The study addresses eight variables: streamflow, groundwater level, precipitation, air temperature, soil moisture, solar radiation, wind speed, and relative humidity. For each variable, a 10-year (2001 to 2010) daily time-series data were retrieved from weather and hydrologic stations selected across Oklahoma. The methodology entailed three phases, including a variable rescaling, a probability analysis, and a divergence quantification. Hence, daily time-series of the selected variables were rescaled to weekly, biweekly, monthly, bimonthly, and trimonthly scales. To derive the probability density function of each variable, a kernel density estimator was applied to the rescaled time-series. The Kullback–Leibler divergence was used to evaluate the deviations pertaining to the time-space scaling. Results showed meaningful divergences that were a consequence of time-space scale variations. However, the sensitivity of variables to the scaling framework differed. For instance, air temperature was less sensitive to time-space scaling, while wind speed, soil moisture, and precipitation were highly sensitive. Correlation analysis showed that correlations tended to gradually increase with the increase in scale, even though the strength of the relation varied, depending on the variable involved. The methodology was tested via a case study where data obtained from a location outside of the study region were used to address the scaling effect on the Normalized Difference Vegetation Index’s response to precipitation and soil moisture. It was concluded that understanding the divergences associated with time-space scales was critical for interpreting results in water resource studies. |