scholarly journals Application of harmonic analysis to ground heat flux determination by creating an artificial fundamental period

2019 ◽  
Vol 28 (6) ◽  
pp. 471-486
Author(s):  
Hans-Dieter Wizemann ◽  
Volker Wulfmeyer ◽  
Thilo Streck
2020 ◽  
Vol 591 ◽  
pp. 125578
Author(s):  
Baoqiang Wu ◽  
Steven P. Oncley ◽  
Huiling Yuan ◽  
Fei Chen

Author(s):  
A. Usman ◽  
B. B. Ibrahim ◽  
L. A. Sunmonu

Characteristic variation of ground heat flux and net radiation enhances the understanding of the significance of indicated trends of variability to everyday life and factors that might be responsible for such variations. This research work critically analyses some specific days with field data over grass-covered surface at Ile-Ife, Nigeria between ground heat flux and net radiation. For the field observations, an instrumented meteorological mast was set up at an experimental site (7°33’N, 4°35’E) located at Obafemi Awolowo University campus, Ile-Ife, Nigeria for a period of two weeks (31st May-14th June, 2013). The soil heat flux, net radiation and soil temperature from the soil heat flux plate; an all-wave net radiometer, and soil thermometer were recorded every 10 seconds and averaged over 2 minutes interval. The sampled data was stored in the data logger (Campbell Scientific, Model CR10X) storage module. After the removal of spurious measurement values (Quality Assurance and Quality Control), the data stored was further reduced to 30 minutes averages using the Microcal Origin (version 7.0) data analysis software. The results showed that the measured ground heat flux, HGM during the daytime increases until 1400 hrs with maximum value of about 136.86 Wm-2 and minimum value of about -72.87 Wm-2 at 0830 hrs (DOY 156). The measured net radiation, Rn value of 649.65 Wm-2 observed at 1400 hrs (DOY 156), represented the maximum value for the entire period of the study. -10.75 Wm-2 value observed at1800 hrs (DOY 154), represented the minimum value for the entire period of the study due to the cloudy condition of the sky which reduces the amount of incoming solar radiation reaching the earth surface.


1995 ◽  
Vol 21 ◽  
pp. 144-148
Author(s):  
Garth W. Paltridge ◽  
Christopher M. Zweck

A simple steady-state energy and mass-balance model of the Antarctic ice sheet is developed. Basically it is a set of two equations with two unknowns of steady-state height h and potential basal temperature Tb. Tb determines whether, and to what extent, there is liquid water at the base of the ice which in turn affects the values of h and Tb. Simultaneous changes of sea-level temperature and precipitation (changes related to each other as might be expected from global climate models) indicate a maximum in the field of possible steady-state ice volumes which may not be far from the presently observed conditions. The possibility of cyclical variation in ground heat flux associated with convection of water and heat in the continental crust is discussed. The mechanism might be capable of generating cycles of ice-sheet volume with relatively short periods similar to those of Milankovitch forcing.


Measurement ◽  
2019 ◽  
Vol 139 ◽  
pp. 1-9 ◽  
Author(s):  
Pedro Jesús Rodríguez de Rivera ◽  
Miriam Rodríguez de Rivera ◽  
Fabiola Socorro ◽  
Manuel Rodríguez de Rivera

2016 ◽  
Vol 25 (5) ◽  
pp. 607-620 ◽  
Author(s):  
Jan-Peter Schulz ◽  
Gerd Vogel ◽  
Claudia Becker ◽  
Steffen Kothe ◽  
Udo Rummel ◽  
...  

2012 ◽  
Vol 48 (8) ◽  
pp. 1367-1374 ◽  
Author(s):  
Robert Pastuszko ◽  
Mieczyslaw E. Poniewski ◽  
Monika Koziol

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