87   Artículos

 
en línea
Vanessa de Arruda Souza, Débora Regina Roberti, Anderson Luis Ruhoff, Tamíres Zimmer, Daniela Santini Adamatti, Luis Gustavo G. de Gonçalves, Marcelo Bortoluzzi Diaz, Rita de Cássia Marques Alves and Osvaldo L. L. de Moraes    
Evapotranspiration (ET) is an important component of the hydrological cycle. Understanding the ET process has become of fundamental importance given the scenario of global change and increasing water use, especially in the agricultural sector. Determinin... ver más
Revista: Water    Formato: Electrónico

 
en línea
Yue Sun, Xiaohong Shi, Shengnan Zhao, Guohua Li, Biao Sun and Jussi Huotari    
It is imperative to elucidate the process of evaporation in lakes, particularly those that are freshwater and are situated in middle and high latitudes. Based on one-year evaporation and high-frequency meteorological?water quality data of Lake Wuliangsuh... ver más
Revista: Water    Formato: Electrónico

 
en línea
Tiffany A. Aldworth, Michele L. W. Toucher, Alistair D. Clulow and Anthony M. Swemmer    
Over the past century, increases in indigenous woody plant species, also known as woody encroachment (WE), has occurred in grasslands and savannas across the globe. While the impact on grassland and savanna composition and productivity has been well stud... ver más
Revista: Hydrology    Formato: Electrónico

 
en línea
Yanxue Liu and Changlu Qiao    
Measuring evapotranspiration (ET) components in cotton fields under mulched drip irrigation is needed to improve water use efficiency and promote the development of water-saving agriculture. In this study, an Eddy Covariance (EC) system was used to obser... ver más
Revista: Agriculture    Formato: Electrónico

 
en línea
Qiongfang Ma, Chaofan Zhang, Ling Chen, Mingyuan Yao, Fan Yang, Hong Yan and Wei Li    
This study observed the characteristics and influencing factors of the carbon fluxes of the Momoge salt marsh ecosystem over four years, which behaves as a CO2 sink. The daily, seasonal, and interannual variations in CO2 fluxes in the Momoge salt marshes... ver más
Revista: Applied Sciences    Formato: Electrónico

 
en línea
Cheng-I Hsieh, I-Hang Huang and Chun-Te Lu    
Canopy resistance is a key parameter in the Penman?Monteith (P?M) equation for calculating evapotranspiration (ET). In this study, we compared a machine learning algorithm?support vector machine (SVM) and an analytical solution (Todorovic, 1999) for esti... ver más
Revista: Water    Formato: Electrónico

 
en línea
Haonan Guo, Shaoyong Wang, Xiaobo He, Yongjian Ding, Yawei Fan, Hui Fu and Xiaofeng Hong    
The Qinghai?Tibet Plateau (QTP), known as the Earth?s third pole, is highly sensitive to climate change. Various environmental degradation has occurred due to the effects of climate warming such as the degradation of permafrost and the thickening of acti... ver más
Revista: Water    Formato: Electrónico

 
en línea
Francisca Aguirre, Oscar Hartogensis, Francisco Meza and Francisco Suárez    
Evapotranspiration (ET) is a critical component of the hydrological cycle, and it links water and energy budgets in the form of latent heat (LvE) released into the atmosphere. However, ET is difficult to measure and is not always well described in arid r... ver más
Revista: Water    Formato: Electrónico

 
en línea
Xiaopei Tang, Haijun Liu, Li Yang, Lun Li and Jie Chang    
Understanding the impact of sprinkler irrigation on field energy balance, microclimate, and crop evapotranspiration is of great importance for optimizing irrigation scheduling and enhancing crop growth. In this study, the microclimate variables, energy, ... ver más
Revista: Agriculture    Formato: Electrónico

 
en línea
Felix Witt, Javis Nwaboh, Henning Bohlius, Astrid Lampert and Volker Ebert    
Water vapor fluxes play a key role in the energy budget of the atmosphere, and better flux measurements are needed to improve our understanding of the formation of clouds and storms. Large-scale measurements of these fluxes are possible by employing the ... ver más
Revista: Applied Sciences    Formato: Electrónico

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