scholarly journals ASSESSMENT OF THERMOCOUPLE TEMPERATURE MEASUREMENTS DURING IN SITU HEATER EXPERIMENTS AT STRIPA, SWEDEN

1985 ◽  
Author(s):  
E. Binnall ◽  
M. McEvoy

2001 ◽  
Author(s):  
B. M. Fichera ◽  
R. L. Mahajan ◽  
T. W. Horst

Abstract Accurate air temperature measurements made by surface meteorological stations are demanded by climate research programs for various uses. Heating of the temperature sensor due to inadequate coupling with the environment can lead to significant errors. Therefore, accurate in-situ temperature measurements require shielding the sensor from exposure to direct and reflected solar radiation, while also allowing the sensor to be brought into contact with atmospheric air at the ambient temperature. The difficulty in designing a radiation shield for such a temperature sensor lies in satisfying these two conditions simultaneously. In this paper, we perform a computational fluid dynamics analysis of mechanically aspirated radiation shields (MARS) to study the effect of geometry, wind speed, and interplay of multiple heat transfer processes. Finally, an artificial neural network model is developed to learn the relationship between the temperature error and specified input variables. The model is then used to perform a sensitivity analysis and design optimization.



Author(s):  
Meenu Ahlawat ◽  
Bachir Saoudi ◽  
Elton Soares de Lima Filho ◽  
Michael R. Wertheimer ◽  
Raman Kashyap




1988 ◽  
Vol 34 (117) ◽  
pp. 178-182 ◽  
Author(s):  
B. Lyle Hansen ◽  
N. S. Gundestrup

AbstractThe 2037 m deep bore hole at Dye 3 in south Greenland was surveyed in 1981, 1983, 1985, and 1986. The directional surveys show the ice flow is planar with a surface velocity of 12.2m/year at an azimuth of 060°, which agrees with surface velocity measured by navigation satellites. Measurements of hole diameter and inclination are highly correlated with dust content in the ice. The temperature measurements show strong convection in the hole fluid with a cell height of about 20 m and an amplitude of 0.1 K. The calculated meanin-situice density is 921.3 ± 1.5kg/m3. Due to ice deformation, the lowest 4 m of the hole were not accessible in 1985 and the lowest 180 m were not accessible in 1986.



2017 ◽  
Vol 190 (3) ◽  
pp. 393-408 ◽  
Author(s):  
Liuhao Ma ◽  
Hongbo Ning ◽  
Junjun Wu ◽  
Wei Ren




2020 ◽  
Vol 68 (4) ◽  
Author(s):  
Makoto Miyajima ◽  
Kazuyuki Kitamura ◽  
Keishi Matsumoto ◽  
Kazuyuki Yagi


2012 ◽  
Vol 100 (20) ◽  
pp. 201112 ◽  
Author(s):  
Michael R. Wertheimer ◽  
Meenu Ahlawat ◽  
Bachir Saoudi ◽  
Raman Kashyap


1980 ◽  
Vol 51 (10) ◽  
pp. 5260 ◽  
Author(s):  
D. D. Bloomquist ◽  
S. A. Sheffield


1951 ◽  
Vol 32 (6) ◽  
pp. 214-216
Author(s):  
Robert L. Denton

A sensitive amplifier is described which can be used, in conjunction with a milliammeter, to measure the low voltages encountered in thermocouple temperature measurements. It is much faster in response and more accurate than conventional bourdon tube type thermographs. The virtual absence of either the zero or sensitivity drift, so common in some types of d.c. amplifiers, and the use of battery power make it particularly useful for recording or indicating in remote locations where it must operate unattended.



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