Effect of diurnal temperature change on cardiovascular risks differed under opposite temperature trends

Author(s):  
Pan Ma ◽  
Ying Zhang ◽  
Xinzi Wang ◽  
Xingang Fan ◽  
Lei Chen ◽  
...  
1991 ◽  
Vol 18 (12) ◽  
pp. 2253-2256 ◽  
Author(s):  
Thomas R. Karl ◽  
George Kukla ◽  
Vyacheslav N. Razuvayev ◽  
Michael J. Changery ◽  
Robert G. Quayle ◽  
...  

2013 ◽  
Vol 26 (22) ◽  
pp. 8765-8780 ◽  
Author(s):  
Yan Li ◽  
Lijuan Zhu ◽  
Xinyi Zhao ◽  
Shuangcheng Li ◽  
Yan Yan

Abstract The impact of urbanization on temperature trends in China was investigated with emphasis on two aspects of urbanization, land cover change, and human activity. A new station classification scheme was developed to incorporate these two aspects by utilizing land cover and energy consumption data. Observation temperature data of 274 stations and National Centers for Environmental Prediction (NCEP)–National Center for Atmospheric Research (NCAR) reanalysis temperature from 1979 to 2010 were used in conducting the observation minus reanalysis (OMR) method to detect urban influence. Results indicated that nearly half of the stations in the study area have been converted from nonurban to urban stations as a result of land cover change associated with urban expansion. It was determined that both land cover change and human activity play important roles in temperature change and contribute to the observed warming, particularly in urbanized stations, where the highest amount of warming was detected. Urbanized stations showed higher OMR temperature trends than those of unchanged stations. In addition, a statistically significant positive relationship was detected between human activity and temperature trends, which suggests that the observed warming is closely related to the intensity and spatial extent of human activity. In fact, the urbanization effect is strongly affected by specific characteristics of urbanization in local and regional scales.


1953 ◽  
Vol 34 (3) ◽  
pp. 106-110 ◽  
Author(s):  
Francis S. Johnson

The heating effect due to absorption of solar energy by atmospheric ozone was calculated from direct measurements of ozone concentrations and of the ultraviolet spectral intensity of sunlight made during a rocket flight over New Mexico on June 14, 1949. Assuming a constant rate of heat loss throughout the day and night due to infrared emission, and no temperature change from day to day, the diurnal temperature change was found to have maximum value of 5.3 C° at 48 km, falling to 1 C° at 31 km and 70 km.


HortScience ◽  
2003 ◽  
Vol 38 (3) ◽  
pp. 387-389 ◽  
Author(s):  
Chad E. Husby ◽  
Alexander X. Niemiera ◽  
J. Roger Harris ◽  
Robert D. Wright

This study was conducted to determine the effects of temperature on nutrient release patterns of three polymer-coated fertilizers (PCFs), each using a different coating technology: Osmocote Plus 15N-3.93P-9.96K, Polyon 18N-2.62P-9.96K, and Nutricote 18N-2.62P-6.64K. Each fertilizer was placed in a sand-filled column and leached with distilled water at ≈100 mL·h-1, while being subjected to a simulated diurnal container temperature change from 20 to 40 °C and back to 20 °C over a period of 20 hours. Column leachate was collected hourly and measured for soluble salts and NO3-N and NH4-N content. For all fertilizers, nutrient release increased and decreased with the respective increase and decrease in temperature. Nutrient release patterns of the three fertilizers differed, with Osmocote Plus showing the greatest overall change in nutrient release between 20 and 40 °C, and Nutricote the least.


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