High atmospheric pressure and accompanying cold season weather types in Poland (1951-2010)

2016 ◽  
Vol 67 (2) ◽  
pp. 165-177 ◽  
Author(s):  
K Piotrowicz ◽  
Z Bielec-Bąkowska ◽  
P Domonkos
Keyword(s):  
Atmospheric Pressure ◽  
Cold Season ◽  
Weather Types ◽  
High Atmospheric Pressure

Growth of Ornamental Plants in Compacted Soils in Relation to Root Growth under Low Oxygen and High Atmospheric Pressure

HortScience ◽  
1998 ◽  
Vol 33 (3) ◽  
pp. 479d-479
Author(s):  
Michael Knee ◽  
Ruth Brake
Keyword(s):  
Atmospheric Pressure ◽  
Root Elongation ◽  
Native Plants ◽  
Tagetes Patula ◽  
Low Oxygen ◽  
Compacted Soils ◽  
Bedding Plants ◽  
Four Levels ◽  
Physical Resistance ◽  
High Atmospheric Pressure

In urban situations, particularly after construction, herbaceous ornamentals may be planted into soils that are compacted or have poor structure so that plant roots may encounter poor aeration or physical resistance. Low oxygen concentrations may be the most important aspect of poor aeration and are readily reproduced in the laboratory. High atmospheric pressure might be used to screen for the ability to grow against physical resistance. We tested the suggestion that “native” plants would grow better in compacted soils than typical bedding plants and for differences in tolerance to low oxygen or high pressure. Plants were grown from seed in the greenhouse at four levels of compaction in peat-based medium and in field soil. Shoot dry weights of the native plants Asclepias tuberosa, Echinacea purpurea, and Schizachyrium scoparius, were less affected by growth in compacted soil or peat medium than those of the bedding plants, Antirrhinum majus, Gypsophila elegans, Impatiens balsamina, Tagetes patula and Zinnia elegans. The oxygen content of media declined with compaction to a minimum of 10 kPa. Half maximal root elongation was observed at 1 to 3 kPa oxygen for most species without any separation between the groups. A presure of 1100 kPa reduced root elongation of the bedding plants by 50 to 70% but only 5 to 20% for the native plants.

Influence of high atmospheric pressure on flame spread over electric wire at different inclinations

2020 ◽  
Vol 136 ◽  
pp. 66-75 ◽  
Author(s):  
Yanli Zhao ◽  
Jian Chen ◽  
Xiao Chen ◽  
Youjie Sheng ◽  
Shouxiang Lu ◽  
...  
Keyword(s):  
Flame Spread ◽  
Atmospheric Pressure ◽  
High Atmospheric Pressure

scholarly journals Variability of the Cold Season Climate in Central Asia. Part I: Weather Types and Their Tropical and Extratropical Drivers

2018 ◽  
Vol 31 (18) ◽  
pp. 7185-7207 ◽  
Author(s):  
Lars Gerlitz ◽  
Eva Steirou ◽  
Christoph Schneider ◽  
Vincent Moron ◽  
Sergiy Vorogushyn ◽  
...  
Keyword(s):  
Central Asia ◽  
Regional Climate ◽  
Cold Season ◽  
Weather Types ◽  
Near Surface ◽  
Climate Conditions ◽  
Temperature Changes ◽  
Central Asian ◽  
Surface Climate ◽  
Moisture Fluxes

To understand the atmospheric mechanisms resulting in a pronounced cold season climate variability in central Asia, an objective weather-type classification is conducted, utilizing a k-means-based clustering approach applied to 500-hPa geopotential height (GPH) fields. Eight weather types (WT) are identified and analyzed with regard to characteristic pressure patterns and moisture fluxes over Eurasia and specific near-surface climate conditions over central Asia. To identify remote drivers of the central Asian climate, WT frequencies are analyzed for their relationships with tropical and extratropical teleconnection modes. The results indicate an influence of Northern Hemispheric planetary wave tracks on westerly moisture fluxes with positive anomalies of precipitation associated with the formation of a Rossby trough over central Asia. Particularly the propagation of the east Atlantic–western Russia and the Scandinavian patterns is shown to modulate regional climate conditions. Variations of ENSO are shown to affect the frequency of particular WTs because of the formation of an anticyclonic anomaly over the Indian Ocean and an increase of tropical fluxes of moisture and heat into central Asia during El Niño events. Further a WT internal influence of ENSO is distinctly defined, with enhanced moisture supply during the ENSO warm phase. The analysis of climatic trends shows that 50% of observed temperature changes can be assigned to variations of the WT composition, indicating that most likely changing regional circulation characteristics account for the enhanced warming rates in central Asia. Trends of precipitation sums are likewise shown to be associated with changing WT frequencies, although the WT–precipitation relationships include large uncertainties.

scholarly journals The impact of high and low atmospheric pressure in the Jordanian environment on some physiological variable for runners .

2013 ◽  
Vol 4 (2) ◽  
pp. 364
Author(s):  
Baker Thnibat
Keyword(s):  
Oxygen Consumption ◽  
Energy Expenditure ◽  
Atmospheric Pressure ◽  
Oxygen Consumption Rate ◽  
Consumption Rate ◽  
Maximal Oxygen Consumption ◽  
Training Groups ◽  
Low Atmospheric Pressure ◽  
The Impact ◽  
High Atmospheric Pressure

<p>The study aimed at identifying the impact of difference between the areas of high atmospheric pressure in the Jordanian environment on some physiological variable ( estimating maximal oxygen consumption , estimating rate of Energy expenditure, and hemoglobin ,vital capacity), for runners .</p><p>  The study sample consisted of (16) athletes who practice ( middle and long – distance running). A number of statistical methods were used to answer the questions of the study ( arithmetic means , standard deviations , Mann.Whiteny test ,and the result of Kolmogorov – Smirnov tests ) .</p><p>  The study result concluded that there was apriority for the measurements which were conducted on the training groups of low atmospheric pressure in comparison with the other group, with regard to the  variables (maximal oxygen consumption , rate of Energy expenditure, and hemoglobin). The study result also showed that there was apriority for the measurements which were conducted on the training groups of high  atmospheric pressure in comparison with the other group, regarding  to the  variables (maximal oxygen consumption , rate of Energy expenditure, and hemoglobin).in the areas of high  atmospheric pressure.</p><p>The study result also suggested that ther were no statistically significant differences between two training groups with regard to the study variables of (maximal oxygen consumption , rate of Energy expenditure, and hemoglobin ,vital capacity), were measured in  of high atmospheric pressure areas .</p><p>The study recommended about building sports facilities that simulate the areas of low atmospheric pressure , because of the expected role that the factors would play in improving some physiological variables .</p>

scholarly journals Atmospheric circulation influence on the interannual variability of snow pack in the Spanish Pyrenees during the second half of the 20th century

2007 ◽  
Vol 38 (1) ◽  
pp. 33-44 ◽  
Author(s):  
Juan I. López-Moreno ◽  
Sergio M. Vicente-Serrano
Keyword(s):  
Atmospheric Circulation ◽  
20Th Century ◽  
Large Scale ◽  
Spatial Scales ◽  
Cold Season ◽  
Snow Accumulation ◽  
Positive Trend ◽  
Snow Pack ◽  
Weather Types ◽  
Spanish Pyrenees

Large areas in the Spanish Pyrenees are covered by snow between December and April, especially above 1650 m a.s.l., the location of the cold season 0°C isotherm. However, a significant negative trend in Pyrenean snow pack was detected during the second half of the 20th century. This paper analyses the interannual evolution of snow accumulation in these mountains in relation to the variability of atmospheric circulation. The study considers two spatial scales, from weather types over the Iberian Peninsula to hemispheric atmospheric patterns. The results show strong relationships between the annual occurrence of several weather types and spring snow accumulation. Changes in the frequency of several weather types are explained by the evolution of large scale hemispheric circulation patterns, especially the North Atlantic Oscillation (NAO). Thus, the positive trend observed in the NAO index leads to a decrease in the occurrence of types that favour snow accumulation and an increase in unfavourable conditions for snow pack during the second half of the 20th century.

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