Vascular convection of heat from active muscle to overlying skin

1959 ◽  
Vol 14 (2) ◽  
pp. 207-211 ◽  
Author(s):  
Theodore Cooper ◽  
Walter C. Randall ◽  
Alrick B. Hertzman
Keyword(s):  
Temperature Gradient ◽  
Surface Temperature ◽  
Temperature Rise ◽  
Active Muscle ◽  
Temperature Changes ◽  
Contracting Muscle ◽  
Arterial Perfusion ◽  
Arterial Dilation ◽  
Absence Of Evidence

Both thermocouple and radiometer measurements revealed marked elevations in temperature of skin immediately over actively working muscles of the forearm and leg. Such localized increases in the surface temperature were confined to skin overlying rhythmically contracting muscle. They were attributed to a direct vertical vascular convection of heat from the muscle to the overlying skin because they were prevented by blocking perfusion or by surgical severance of skin from underlying tissue and because of the character of the temperature gradient in the intervening tissue. The argument for a venous rather than an arterial convection was based on a) the effects of compression of the superficial veins on the temperature changes, b) the absence of effect on the latter by electrophoresis of adrenaline into the skin, which greatly reduced arterial perfusion of the skin, c) the absence of evidence of arterial dilation in the skin and d) the lack of relation of the location of arterial twigs to the topography of the temperature rise. Submitted on August 11, 1958

Application of pyrometer and standard sample to determine surface temperature of studied materials

2019 ◽  
pp. 9-13
Author(s):  
V.Ya. Mendeleyev ◽  
V.A. Petrov ◽  
A.V. Yashin ◽  
A.I. Vangonen ◽  
O.K. Taganov
Keyword(s):  
Composite Material ◽  
Surface Temperature ◽  
Relative Error ◽  
Wavelength Range ◽  
Standard Sample ◽  
A Priori ◽  
Temperature Changes ◽  
Surface Temperatures ◽  
Relative Errors ◽  
Normal Emissivity

Determining the surface temperature of materials with unknown emissivity is studied. A method for determining the surface temperature using a standard sample of average spectral normal emissivity in the wavelength range of 1,65–1,80 μm and an industrially produced Metis M322 pyrometer operating in the same wavelength range. The surface temperature of studied samples of the composite material and platinum was determined experimentally from the temperature of a standard sample located on the studied surfaces. The relative error in determining the surface temperature of the studied materials, introduced by the proposed method, was calculated taking into account the temperatures of the platinum and the composite material, determined from the temperature of the standard sample located on the studied surfaces, and from the temperature of the studied surfaces in the absence of the standard sample. The relative errors thus obtained did not exceed 1,7 % for the composite material and 0,5% for the platinum at surface temperatures of about 973 K. It was also found that: the inaccuracy of a priori data on the emissivity of the standard sample in the range (–0,01; 0,01) relative to the average emissivity increases the relative error in determining the temperature of the composite material by 0,68 %, and the installation of a standard sample on the studied materials leads to temperature changes on the periphery of the surface not exceeding 0,47 % for composite material and 0,05 % for platinum.

Core and body surface temperature changes during sledge hockey competition

2017 ◽  
Vol 26 (2) ◽  
pp. 1037-1044
Author(s):  
Eu-Jin Jung ◽  
Lae-Guen Jang ◽  
Geun-Hoon Choi ◽  
Hyon Park
Keyword(s):  
Surface Temperature ◽  
Body Surface ◽  
Temperature Changes ◽  
Body Surface Temperature

scholarly journals Cities Exacerbate Climate Warming

Urban Science ◽  
2021 ◽  
Vol 5 (1) ◽  
pp. 27
Author(s):  
Lahouari Bounoua ◽  
Kurtis Thome ◽  
Joseph Nigro
Keyword(s):  
Surface Temperature ◽  
Land Surface ◽  
Large Scale ◽  
Climate Models ◽  
Warming Trend ◽  
Climate Mitigation ◽  
Temperature Changes ◽  
Surface Warming ◽  
The Us

Urbanization is a complex land transformation not explicitly resolved within large-scale climate models. Long-term timeseries of high-resolution satellite data are essential to characterize urbanization within land surface models and to assess its contribution to surface temperature changes. The potential for additional surface warming from urbanization-induced land use change is investigated and decoupled from that due to change in climate over the continental US using a decadal timescale. We show that, aggregated over the US, the summer mean urban-induced surface temperature increased by 0.15 °C, with a warming of 0.24 °C in cities built in vegetated areas and a cooling of 0.25 °C in cities built in non-vegetated arid areas. This temperature change is comparable in magnitude to the 0.13 °C/decade global warming trend observed over the last 50 years caused by increased CO2. We also show that the effect of urban-induced change on surface temperature is felt above and beyond that of the CO2 effect. Our results suggest that climate mitigation policies must consider urbanization feedback to put a limit on the worldwide mean temperature increase.

scholarly journals The relevance of mid-Holocene Arctic warming to the future

2019 ◽  
Vol 15 (4) ◽  
pp. 1375-1394 ◽  
Author(s):  
Masakazu Yoshimori ◽  
Marina Suzuki
Keyword(s):  
Surface Temperature ◽  
General Circulation ◽  
Temperature Response ◽  
Longwave Radiation ◽  
General Circulation Models ◽  
Cross Model ◽  
Arctic Warming ◽  
Temperature Changes ◽  
The Future ◽  
Arctic Climate Change

Abstract. There remain substantial uncertainties in future projections of Arctic climate change. There is a potential to constrain these uncertainties using a combination of paleoclimate simulations and proxy data, but such a constraint must be accompanied by physical understanding on the connection between past and future simulations. Here, we examine the relevance of an Arctic warming mechanism in the mid-Holocene (MH) to the future with emphasis on process understanding. We conducted a surface energy balance analysis on 10 atmosphere and ocean general circulation models under the MH and future Representative Concentration Pathway (RCP) 4.5 scenario forcings. It is found that many of the dominant processes that amplify Arctic warming over the ocean from late autumn to early winter are common between the two periods, despite the difference in the source of the forcing (insolation vs. greenhouse gases). The positive albedo feedback in summer results in an increase in oceanic heat release in the colder season when the atmospheric stratification is strong, and an increased greenhouse effect from clouds helps amplify the warming during the season with small insolation. The seasonal progress was elucidated by the decomposition of the factors associated with sea surface temperature, ice concentration, and ice surface temperature changes. We also quantified the contribution of individual components to the inter-model variance in the surface temperature changes. The downward clear-sky longwave radiation is one of major contributors to the model spread throughout the year. Other controlling terms for the model spread vary with the season, but they are similar between the MH and the future in each season. This result suggests that the MH Arctic change may not be analogous to the future in some seasons when the temperature response differs, but it is still useful to constrain the model spread in the future Arctic projection. The cross-model correlation suggests that the feedbacks in preceding seasons should not be overlooked when determining constraints, particularly summer sea ice cover for the constraint of autumn–winter surface temperature response.

Estimating surface temperature changes of lakes in the Tibetan Plateau using MODIS LST data

2014 ◽  
Vol 119 (14) ◽  
pp. 8552-8567 ◽  
Author(s):  
Guoqing Zhang ◽  
Tandong Yao ◽  
Hongjie Xie ◽  
Jun Qin ◽  
Qinghua Ye ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Surface Temperature ◽  
The Tibetan Plateau ◽  
Temperature Changes

Addressing Paraffin Deposition Challenges Through New Technologies

2021 ◽  
Author(s):  
Saugata Gon ◽  
Christopher Russell ◽  
Kasper Koert Jan Baack ◽  
Heather Blackwood ◽  
Alfred Hase
Keyword(s):  
Temperature Gradient ◽  
Surface Temperature ◽  
New Technologies ◽  
Test Methods ◽  
Large Temperature ◽  
Mixing Condition ◽  
Cold Finger ◽  
Cold Surface ◽  
Bulk Oil ◽  
Conventional Test

Abstract Paraffin deposition is a common challenge for production facilities globally where production fluid/process surface temperature cools down and reach below the wax appearance temperature (WAT) of the oil. Although chemical treatment is used widely for suitable mitigation of wax deposition, conventional test methods like cold finger often fail to recommend the right product for the field. The current study will present development of two new technologies PARA-Window and Dynamic Paraffin Deposition Cell (DPDC)to address such limitations. Large temperature gradient between bulk oil and cold surface has been identified as a major limitation of cold finger. To address this, PARA-Window has been developed to capture the paraffin deposition at a more realistic temperature gradient (5°C) between the bulk oil and surface temperature using a NIR optical probe. Absence of brine and lack of shear has been identified as another limitation of cold finger technique. DPDC has been developed to study paraffin deposition and chemical effectiveness in presence of brine. Specially designed cells are placed horizontally inside a shaker bath to achieve good mixing between oil and water for DPDC application. A prior study by Russell et al., (2019) showed the effectiveness of PARA-Window in capturing deposition phenomena of higher molecular weight paraffin chains that resemble closely to field deposits under narrow temperature gradient around WAT. Conventional test methods fail to capture meaningful product differentiation in most oils under such conditions and hence can only recommend a crystal modifier type of paraffin chemistries. PARA-Window technique can expand product selection to other type of paraffin chemistries (paraffin crystal modifiers, dispersants and solvents) as shown earlier by Russell et al., (2021). The usage of DPDC allows us to create a dynamic mixing condition inside the test cells with both oil and water under a condition similar to production pipe systems. This allows DPDC to assess water effect on paraffin chemistries (crystal modifiers and dispersants). This study presents the usage of these two new technologies to screen performance of different types of paraffin chemistries on select oils and their advantages over cold finger. The results identify how mimicking field conditions using these new technologies can capture new insights into paraffin products.

Temperature in the external auditory meatus as an index of central temperature changes

1964 ◽  
Vol 19 (5) ◽  
pp. 1032-1034 ◽  
Author(s):  
K. E. Cooper ◽  
W. I. Cranston ◽  
E. S. Snell
Keyword(s):  
Temperature Gradient ◽  
Temperature Regulation ◽  
External Auditory Meatus ◽  
Absolute Temperature ◽  
Central Temperature ◽  
Temperature Changes ◽  
Vasomotor Responses ◽  
Temperature Levels

The temperature of the wall of the external auditory meatus has been investigated. Changes in ear temperature reflect changes of sublingual temperature quite accurately and are well correlated with cutaneous vasomotor responses induced by body heating. The temperature of the external auditory meatus is little affected by reflex vasomotor changes. It is easily measured without discomfort or danger and provides a valid indication of temperature changes at the central receptors. There is a considerable temperature gradient down the wall of the meatus so that absolute temperature levels are probably not of value. ear temperature in man; central temperature regulation in man Submitted on February 24, 1964

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