|
|
|
Jinming Chen, Xiao Yang, Haiya Dao, Haowen Gu, Gang Chen, Changshu Mao, Shihan Bai, Shixiang Gu, Zuhao Zhou and Ziqi Yan
Water, soil, and heat are strategic supporting elements for human survival and social development. The degree of matching between human-land-water-heat elements directly influences the sustainable development of a region. However, the current evaluation ...
ver más
|
|
|
|
|
|
|
Pengxuan Wang, Yixi Wang, Weijun Gao, Tongyu Xu, Xindong Wei, Chunyan Shi, Zishu Qi and Li Bai
In cold regions, due o the impact of climatic conditions, the heat load in winter and the cooling load in summer are unbalanced. In the long-term operation of the ground-source heat pump (GSHP), the soil heat imbalance phenomenon has still not been succe...
ver más
|
|
|
|
|
|
|
Susana Del Pozo, Cristina Sáez Blázquez, Ignacio Martín Nieto and Susana Lagüela
Infrared thermography can be used for the thermal characterization of geothermal environments, through the monitoring of the surface that allows the computation of the thermal imbalance including the three heat transfer methods, consequently estimating t...
ver más
|
|
|
|
|
|
|
Ron Kremser, Niclas Grabowski, Roman Düssel, Albert Mulder and Dietmar Tutsch
In aluminium production, anode effects occur when the alumina content in the bath is so low that normal fused salt electrolysis cannot be maintained. This is followed by a rapid increase of pot voltage from about 4.3 V to values in the range from 10 to 8...
ver más
|
|
|
|
|
|
|
Lijing Cheng, Gongjie Wang, John P. Abraham and Gang Huang
Ocean heat content (OHC) is the major component of the earth’s energy imbalance. Its decadal scale variability has been heavily debated in the research interest of the so-called “surface warming slowdown” (SWS) that occurred during the ...
ver más
|
|
|
|
|
|
|
DANIELE MASSERONI,CHIARA CORBARI,MARCO MANCINI
Pág. 335 - 352
The use of energy fluxes data to validate land surface models requires that energy balance closure conservationis satisfied, but usually this condition is not verified when the available energy is bigger than the sumof turbulent vertical fluxes. In this ...
ver más
|
|
|
|