scholarly journals Contemporary Warming and Daily Values of Temperature (on the Example of Warsaw)

2004 ◽  
Vol 11 (1) ◽  
pp. 119-126
Author(s):  
Urszula Kossowska-Cezak
Keyword(s):  
Air Temperature ◽  
Minimum Temperature ◽  
Daily Temperature ◽  
Maximum Temperature ◽  
Absolute Maximum ◽  
Absolute Minimum ◽  
Mean Temperature ◽  
The Mean ◽  
Minimum Daily Temperature ◽  
Warming Process

Abstract This paper aims at presenting changes in everyday air temperature values, triggered by the contemporary warming process. The analysis has been based on the mean, maximum, and minimum daily temperature values measured in Warsaw between 1951 – 2003. The mean daily temperature in that period was between −24.6 and 28.4°C, absolute minimum temperature was −30.7°C, absolute maximum temperature amounted to 36.4°C. Calculations indicate that the number of days with mean temperature ≤ −5.0°C (minimum < 0.0°C, maximum < 0.0°C) in the last several years decreased. This trend slowed down at the beginning of 21st century, nevertheless, the number of days with mean daily temperature > 20.0°C and maximum temperature > 25.0°C was growing, particularly in the 1990’s and even more so in early 2000’s. Also since 1990’s, there has been increasingly more nights with minimum temperature > 15.0°C, which has been particularly apparent in 2001. Contemporary warming is then marked with an increasing frequency of the hottest days and decreasing frequency of the coldest days. These changes were asymmetrical beyond 1950’s, yet, in late 1990’s they coincided.

scholarly journals Evidence of elevation-dependent warming from the Chinese Tian Shan

2021 ◽  
Vol 15 (12) ◽  
pp. 5765-5783
Author(s):  
Lu Gao ◽  
Haijun Deng ◽  
Xiangyong Lei ◽  
Jianhui Wei ◽  
Yaning Chen ◽  
...  
Keyword(s):  
Air Temperature ◽  
Minimum Temperature ◽  
Swiss Alps ◽  
Maximum Temperature ◽  
Current Evidence ◽  
High Mountain ◽  
Regional Warming ◽  
Mean Temperature ◽  
Warming Rate ◽  
Tian Shan

Abstract. The phenomenon in which the warming rate of air temperature is amplified with elevation is termed elevation-dependent warming (EDW). It has been clarified that EDW can accelerate the retreat of glaciers and melting of snow, which can have significant impacts on the regional ecological environment. Owing to the lack of high-density ground observations in high mountains, there is widespread controversy regarding the existence of EDW. Current evidence is mainly derived from typical high-mountain regions such as the Swiss Alps, the Colorado Rocky Mountains, the tropical Andes and the Tibetan Plateau–Himalayas. Rare evidence in other mountain ranges has been reported, especially in arid regions. In this study, EDW features (regional warming amplification and altitude warming amplification) in the Chinese Tian Shan (CTM) were detected using a unique high-resolution (1 km, 6-hourly) air temperature dataset (CTMD) from 1979 to 2016. The results showed that there were significant EDW signals at different altitudes on different timescales. The CTM showed significant regional warming amplification in spring, especially in March, and the warming trends were greater than those of continental China with respect to three temperatures (minimum temperature, mean temperature and maximum temperature). The significance values of EDW above different altitude thresholds are distinct for three temperatures in 12 months. The warming rate of the minimum temperature in winter showed a significant elevation dependence (p<0.01), especially above 3000 m. The greatest altitudinal gradient in the warming rate of the maximum temperature was found above 4000 m in April. For the mean temperature, the warming rates in June and August showed prominent altitude warming amplification but with different significance above 4500 m. Within the CTM, the Tolm Mountains, the eastern part of the Borokoonu Mountains, the Bogda Mountains and the Balikun Mountains are representative regions that showed significant altitude warming amplification on different timescales. This new evidence could partly explain the accelerated melting of snow in the CTM, although the mechanisms remain to be explored.

scholarly journals Correlation Between Local Air Temperature and the COVID-19 Pandemic in Hubei, China

2021 ◽  
Vol 8 ◽  
Author(s):  
Cheng-yi Hu ◽  
Lu-shan Xiao ◽  
Hong-bo Zhu ◽  
Hong Zhu ◽  
Li Liu
Keyword(s):  
Air Temperature ◽  
Minimum Temperature ◽  
Regression Models ◽  
Hubei Province ◽  
Daily Temperature ◽  
Maximum Temperature ◽  
Influence Of Temperature ◽  
Influence Of Temperature On ◽  
Almost All

Objective: To clarify the correlation between temperature and the COVID-19 pandemic in Hubei.Methods: We collected daily newly confirmed COVID-19 cases and daily temperature for six cities in Hubei Province, assessed their correlations, and established regression models.Results: For temperatures ranging from −3.9 to 16.5°C, daily newly confirmed cases were positively correlated with the maximum temperature ~0–4 days prior or the minimum temperature ~11–14 days prior to the diagnosis in almost all selected cities. An increase in the maximum temperature 4 days prior by 1°C was associated with an increase in the daily newly confirmed cases (~129) in Wuhan. The influence of temperature on the daily newly confirmed cases in Wuhan was much more significant than in other cities.Conclusion: Government departments in areas where temperatures range between −3.9 and 16.5°C and rise gradually must take more active measures to address the COVID-19 pandemic.

scholarly journals EFEITOS DA VEGETAÇÃO NA VARIAÇÃO TÉRMICA DA CIDADE DE CURITIBA, PR

FLORESTA ◽  
2014 ◽  
Vol 44 (3) ◽  
pp. 451 ◽  
Author(s):  
Luciana Leal ◽  
Daniela Biondi ◽  
Antonio Carlos Batista
Keyword(s):  
Air Temperature ◽  
Urban Climate ◽  
Urban Forestry ◽  
Anthropogenic Heat ◽  
Maximum Temperature ◽  
Absolute Maximum ◽  
Absolute Minimum ◽  
Meteorological Model ◽  
The Absolute ◽  
Autumn And Winter

Considerando que a distribuição das florestas urbanas e o zoneamento do uso do solo influenciam o clima local da cidade de Curitiba, este trabalho teve como objetivo analisar o efeito desses fatores na variação temporal e espacial da temperatura do ar nessa cidade. Os dados de temperatura foram coletados em quatro campanhas em períodos correspondentes às estações do ano em 2011, em 44 pontos de monitoramento em quatro transectos na malha urbana da cidade, por meio de miniabrigos meteorológicos com registradores modelo Hobo®. Nos quatro transectos, foram observadas diferenças térmicas entre os pontos de monitoramento nos períodos analisados. Para a temperatura máxima absoluta, as diferenças foram de até 5,8 ºC no transecto sudoeste-nordeste, e para a temperatura mínima absoluta, de 4,6 ºC no transecto noroeste-sudeste. Mesmo nas estações do ano de mais baixas temperaturas, outono e inverno, foram encontradas diferenças térmicas, relacionadas ao calor antropogênico. As maiores temperaturas foram encontradas nos locais com maior intensidade de ocupação e atividades antrópicas, porém não nas áreas mais verticalizadas, enquanto as menores temperaturas foram encontradas nas regiões com maior quantidade de áreas permeáveis, concentração de remanescentes florestais ou espaços verdes públicos, confirmando a influência da densidade de construção e da presença de vegetação na variação das temperaturas na cidade de Curitiba.Palavras-chave:  Clima urbano; temperatura do ar; florestas urbanas; classes de densidade de ocupação. AbstractEffects of vegetation on thermal intra-urban variation of Curitiba - PR. Whereas the distribution of urban forests and zoning land use influence the climate of Curitiba city, this research aimed to analyze the effect of this factors in temporal and spatial variation of air temperature in this town. Temperature data were collected in four campaigns in periods corresponding to the seasons of the year in 2011, in 44 monitoring points in four transects in the urban mesh by mini-shields meteorological model with Hobo® loggers. In the four transects were found differences between the thermal monitoring points in the analyzed periods. For the absolute maximum temperature, differences were up to 5.8 ºC in the northeast-southwest transect and the absolute minimum temperature of 4.6 ºC in the northeast-southwest transect. Even in seasons of lower temperatures, autumn and winter, thermal differences were related to anthropogenic heat. The highest temperatures were found in the regions with greater intensity of occupation and human activities, however not in the areas with verticalization, while the lowest temperatures were observed in regions with higher permeable areas, concentration of remaining forest and public green spaces. As result, it confirms the influence of building density and the presence of vegetation in the variation of temperature in the city of Curitiba.Keywords: Urban climate; air temperature; urban forestry; class occupation density.

Observations on 287 thunder-storms made at highfield house, near Nottingham, during the last nine years

1851 ◽  
Vol 5 ◽  
pp. 957-957
Keyword(s):  
Minimum Temperature ◽  
Maximum Temperature ◽  
Tabular Form ◽  
The Hours ◽  
The Mean ◽  
Atmospheric Phenomena ◽  
Rotatory Motion

The thunder-storms referred to in this communication are recorded in a tabular form., arranged according to their dates. In this table are given the date; the hour of the commencement of the storm; the mean height of the barometer to tenths of an inch; whether it is rising, stationary, or falling; the direction of the wind before the storm, during its continuance, and after its cessation; the maximum temperature on the day of the storm and on the day after; the minimum temperature on the night before and on the night after; and general remarks on the storms. This table is followed by remarks on particular storms recorded in it. In conclusion the author gives the results of his observations with reference to the number of storms in each year; the number in each month, with the hours at which they mostly occur in particular months; the number that have occurred with a rising, stationary, or falling barometer; the number in respect to the direction of the wind and of the current in which the storms moved; the number of storms that have occurred at the various heights of the maximum, and also of the minimum thermometer; the number in which the peculiar breeze that suddenly springs up on the commencement of thunder-storms has been well marked; the change in the direction of some of these storms, and indications of rotatory motion; and finally, the different atmospheric phenomena which have accompanied these storms.

THE TEMPERATURES OF SURFACE FIRES IN JACK PINE BARREN: I. THE VARIATION IN TEMPERATURE WITH TIME

1966 ◽  
Vol 44 (10) ◽  
pp. 1285-1292 ◽  
Author(s):  
David W. Smith ◽  
John H. Sparling
Keyword(s):  
Jack Pine ◽  
Maximum Temperature ◽  
Surface Fires ◽  
Mean Temperature ◽  
The Mean ◽  
Maximum Temperatures

The temperatures of 18 fires in an open jack pine barren near Timmins, Ontario, have been recorded. The maximum temperature recorded was 545 °C, although in other determinations fire temperatures in excess of 1000 °C were reached. The mean temperature of all fires was 340.6 ± 133.2 °C. Three fires at 230, 345, and 545 °C were considered in detail.The maximum temperature of a fire was normally recorded at heights of 5 cm or 10 cm above the surface. Maximum temperatures of hotter fires usually occurred at greater heights than cooler ones. Duration and the temperature ("intensity") of the fire are important aspects of fire studies.

scholarly journals Temperature Change and Its Elevation Dependency in the Source Region of the Yangtze River and Yellow River

2014 ◽  
Vol 6 (2) ◽  
pp. 124 ◽  
Author(s):  
Chongyi E ◽  
Hongchang Hu ◽  
Hong Xie ◽  
Yongjuan Sun
Keyword(s):  
Temperature Change ◽  
Minimum Temperature ◽  
Yangtze River ◽  
Yellow River ◽  
Source Region ◽  
Maximum Temperature ◽  
Climatic Data ◽  
The Yangtze River ◽  
Extreme Minimum Temperature ◽  
The Mean

The study of temperature change and its elevation dependency in the source region of the Yangtze River and Yellow River have been insufficient owing to the lack of adequate observation stations and long-term climatic data. In this study five temperature indices of 32 stations from 1961 to 2007 in and near the source region are used. The 32 stations all have experienced significant warming; the warming amplitudes are higher than the mean warming amplitude of the Qinghai-Tibetan plateau. The warming amplitudes and the numbers of stations showing significant warming trends in mean minimum temperature and extreme minimum temperature are higher than that of the mean maximum temperature and extreme maximum temperature. The elevation dependency of climatic warming and the amount of significant warming stations are not obvious; the influence of human activity and urbanization may be higher. The warming amplitudes of 26 stations above 3000 m tend to be uniform, and there is no significant law at 6 stations below 3000 m. On the contrary, the ratio of stations showing significant warming in minimum temperature above 4000 m is far less than that of the stations below 4000 m.

A study about the linearity of trends between extreme and mean temperatures in Argentina

2021 ◽  
Author(s):  
Solange Suli ◽  
Matilde Rusticucci ◽  
Soledad Collazo
Keyword(s):  
Linear Regression ◽  
Linear Relationship ◽  
Statistical Significance ◽  
Coefficient Of Determination ◽  
Maximum Temperature ◽  
Mean Temperature ◽  
Change In The Mean ◽  
The Mean ◽  
Student’S T ◽  
Cold Extremes

&lt;p&gt;Small variations in the mean state of the atmosphere can cause large changes in the frequency of extreme events. In order to deepen and extend previous results in time, in this work we analyzed the linear relationship between extreme and mean temperature (&amp;#932;) on a climate change scale in Argentina. Two monthly extreme indices, cold nights (TN10) and warm days (TX90), were calculated based on the quality-controlled daily minimum and maximum temperature data provided by the Argentine National Meteorological Service from 58 conventional weather stations located over Argentina in the 1977&amp;#8211;2017 period. Subsequently, we evaluated the relationship between the linear trends of extremes and mean temperature on a seasonal basis (JFM, AMJ, JAS, and OND). Student's T-test was performed to analyze their statistical significance at 5%. Firstly, positive (negative) and significant linear regressions were found between TX90 (TN10) trends and mean temperature trends for the four studied seasons. Therefore, an increase in the &amp;#932;-trend maintains a linear relationship with significant increase (decrease) of warm days (cold nights). Moreover, we found that JFM was the one with the highest coefficient of determination (0.602 for hot extremes and 0.511 for cold extremes), implying that 60.2% (51.1%) of the TX90 (TN10) trend could be explained as a function of the &amp;#932;-trend by a linear regression. In addition, in the JFM (OND) quarter, the TX90 index increased by 7.02 (6.02) % of days each with a 1 &amp;#186;C increase in the mean temperature. Likewise, the TN10 index decreased by 4.94 (and 4.99) % of days from a 1&amp;#186;C increase in the mean temperature for the JFM (AMJ) quarter. Finally, it is worthwhile to highlight the uneven behavior between hot and cold extremes and the mean temperature. Specifically, it was observed that the slopes of the linear regression calculated for the TX90 index and &amp;#932;&amp;#160;presented a higher absolute value than those registered for the TN10 index and &amp;#932;. Therefore, a change in the mean temperature affects hot extremes to a greater extent than cold ones in Argentina.&lt;/p&gt;

Bioclimate of Jericho in Palestine

2019 ◽  
Vol 7 (1) ◽  
pp. 1-7
Author(s):  
Jehad Ighbareyeh
Keyword(s):  
Minimum Temperature ◽  
Thermal Model ◽  
Arid Regions ◽  
Dead Sea ◽  
Maximum Temperature ◽  
Stone Age ◽  
The Earth ◽  
Latitudinal Belt ◽  
The Mean ◽  
Very High

 Jericho is an ancient Canaanite Palestinian city and one of the oldest cities in history, which dates back to more than 10.000 BC (Stone Age). It is located near to the Jordan River, north of the Dead Sea, and north of Jerusalem. Moreover, it considered the lowest area in the earth and has a unique climatic zone. during the study period (1975-1995), was utilized the Salvador Rivas Martinez scale to classify the bioclimate of the earth to analysis the climate and bioclimate data, which was obtained from one station from Palestinian Meteorology Department (Jericho station). The results revealed that the mean monthly temperature was 22.4 0C, mean maximum temperature was 34.8 0C, mean monthly minimum temperature was 15.3 0C, the value of the annual ombrothermic index was 0.6, the compensated thermicity index is very high around 1209/1209 and the simple continentality index was 16.7. The bioclomate of Jericho is located within the zones of the thermal model under the inframediterranean basin, the dry and arid regions. Jericho is belong to Mediterranean desertic-oceanic, the latitudinal belt as subtropical, while continentality is oceanic-low eu-oceanic.

scholarly journals Ambient temperature correlates with geographic variation in body size of least horseshoe bats

2020 ◽  
Vol 66 (5) ◽  
pp. 459-465 ◽  
Author(s):  
Man Wang ◽  
Kelly Chen ◽  
Dongge Guo ◽  
Bo Luo ◽  
Weiwei Wang ◽  
...  
Keyword(s):  
Body Size ◽  
Geographic Variation ◽  
Body Mass ◽  
Body Length ◽  
Primary Productivity ◽  
Minimum Temperature ◽  
Maximum Temperature ◽  
Heat Conservation ◽  
The Mean ◽  
Horseshoe Bats

Abstract Geographic variation in body size is common within many animal species. The causes of this pattern, however, remain largely unexplored in most vertebrate groups. Bats are widely distributed globally owing to their ability of powered flight. Most bat species encounter a variety of climatic conditions across their distribution range, making them an ideal taxon for the study of ecogeographic patterns in body size. Here, we used adult least horseshoe bats, Rhinolophus pusillus, to test whether geographic variation in body size was determined by heat conservation, heat dissipation, climatic seasonality, or primary productivity. We measured body mass and head-body length for 246 adult bats from 12 allopatric colonies in China. We quantified the ecological conditions inhabited by each colony, including mean maximum temperature of the warmest month, mean minimum temperature of the coldest month, temperature seasonality, precipitation seasonality, and annual net primary productivity (ANPP). Body mass and head-body length, 2 of the most reliable indicators of body size, exhibited marked differences between colonies. After controlling for spatial autocorrelation, the mean minimum temperature of the coldest month explained most of the variation in body size among colonies, regardless of sex. The mean maximum temperature, climatic seasonality, and ANPP had limited power in predicting body size of males or females in comparison with mean minimum temperature. These results support the heat conservation hypothesis and suggest adaptive responses of body size to cold climates in cave-dwelling bats.

Effect of Heat-Reflective Insulation Coating on Exterior Walls of Building Energy Consumption in Summer

2011 ◽  
Vol 105-107 ◽  
pp. 922-925 ◽  
Author(s):  
Chao He ◽  
Wei Lin Guo ◽  
Yi Yun Huang
Keyword(s):  
Energy Saving ◽  
Temperature Change ◽  
Air Temperature ◽  
Heat Insulation ◽  
Maximum Temperature ◽  
Heat Gain ◽  
Insulation Coating ◽  
Building Wall ◽  
The Mean ◽  
Saving Effect

To discuss the effect of energy saving of heat-reflective insulation coating on exterior walls of building, the wall temperature change of two test rooms with heat insulation or not in Hangzhou has been monitored in summer, and the heat flux data of east, south and west walls were analyzed. The results indicate that the temperature of outside wall surface with the heat reflective insulation coating is reduced effectively, and the maximum temperature change was about 9, 10°C. There is a positive proportional between the mean daily air temperature and heat gain that the heat gain increases with the mean daily air temperature. By calculating, the higher the air temperature, the more the cooling effect of coating in summer. But the higher the mean daily temperature do not mean that the more heat gain in summer. The result shows the energy saving effect of the heat insulation coating on building wall was very obvious in summer in Hangzhou.

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