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Journal articles on the topic 'Bioclimatology'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 July 2024

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1

Goward, Samuel N. "Satellite Bioclimatology." Journal of Climate 2, no. 7 (July 1989): 710–20. http://dx.doi.org/10.1175/1520-0442(1989)002<0710:sb>2.0.co;2.

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2

Mayer, H. "Urban bioclimatology." Experientia 49, no. 11 (November 1993): 957–63. http://dx.doi.org/10.1007/bf02125642.

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3

Rui-Zhao, Zhu. "Bioclimatology of frost (Advances in Bioclimatology, Vol. 2)." Boundary-Layer Meteorology 68, no. 3 (March 1994): 329–30. http://dx.doi.org/10.1007/bf00705605.

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4

Newman, James E. "Advances in bioclimatology. Volume 2. The bioclimatology of frost." Agricultural and Forest Meteorology 67, no. 1-2 (December 1993): 147–48. http://dx.doi.org/10.1016/0168-1923(93)90055-m.

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5

Rundquist, Bradley, John Harrington, and Douglas Goodin. "Mesoscale Satellite Bioclimatology." Professional Geographer 52, no. 2 (May 2000): 331–44. http://dx.doi.org/10.1111/0033-0124.00229.

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6

Fuentes, J. D. "Advances in Bioclimatology, Vol. 1." Journal of Environmental Quality 22, no. 4 (October 1993): 870–71. http://dx.doi.org/10.2134/jeq1993.00472425002200040037x.

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7

Jauregui, E. "Urban bioclimatology in developing countries." Experientia 49, no. 11 (November 1993): 964–68. http://dx.doi.org/10.1007/bf02125643.

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8

Black, P. B. "Advances in Bioclimatology, Vol. 2: The Bioclimatology of Frost. Its Occurrence, Impact and Protection." Journal of Environmental Quality 22, no. 3 (July 1993): 635. http://dx.doi.org/10.2134/jeq1993.00472425002200030036x.

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9

Escourrou, Gisèle. "Réflexions sur la notion de stress en bioclimatologie humaine (About the stress in human bioclimatology)." Bulletin de l'Association de géographes français 65, no. 5 (1988): 347–55. http://dx.doi.org/10.3406/bagf.1988.1448.

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10

Valencia-Barrera, Rosa María, Paul Comtois, and Delia Fernández-González. "Biogeography and bioclimatology in pollen forecasting." Grana 40, no. 4-5 (January 2001): 223–29. http://dx.doi.org/10.1080/001731301317223259.

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11

Pecelj, Milovan, Miroljub Milincic, and Milica Pecelj. "Bioclimatology and ecoclimatology prospecting: Right out development." Glasnik Srpskog geografskog drustva 87, no. 2 (2007): 199–210. http://dx.doi.org/10.2298/gsgd0702199p.

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This paper discusses fact that there is small number of articles about bioclimatic research in domestic scientific literature which is correlated with small number of bioclimatic researching projects. Authors want to emphasize that for changing this condition it is necessary to applying multidisciplinary approach to bioclimatic research. As an example of multidisciplinary approach in bioclimatic research it is representing mathematical model MENEX-5. This model opens a new opportunities for bioclimatic research of actual environmental problems, which are trigger by global climate change and destruction of ozone layer.
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12

Abels, D. "Bioclimatology at the Dead Sea in Israel." Clinics in Dermatology 14, no. 6 (December 1996): 653–58. http://dx.doi.org/10.1016/s0738-081x(96)00100-9.

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13

Rajkai, K. "The role of soil in bioclimatology – a review." Soil and Water Research 3, Special Issue No. 1 (June 30, 2008): S30—S41. http://dx.doi.org/10.17221/8/2008-swr.

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Soil’s part in bioclimatology is not defined and formulated yet. We interpret soil together with its plant cover as primary climate modifier for organisms living on, and within it. At the same time evaporating soil together with its transpiring vegetation is affecting the climate, and functioning as secondary climate modifier in context of bioclimatology. Selected Hungarian studies are used to highlight four primary and three secondary soil modifier actions connected to bioclimatology. Both primary and secondary soil modifier roles coupled mainly to soil hydro-physical properties. The first primary soil climate modifier action is the dew formation in the surface of sandy soils. As dew 80 mm of water can annually be transported from the subsoil to soil surface. Positive water resource value of dew is still not completely accepted. The second primary soil climate modifier example presents different amounts of usable soil moisture resource in two oak forest habitats with different species composition of herbs. In the third primary soil example the microclimate of the wetter habitat with deeper soil and denser herb vegetation of the oak forest – estimated by inverse modelling – showed higher shading, air moisture content and lower soil coverage than that of dry one. In the fourth primary soil modifier example forest hydrology is quantified for a Scots pine forest. Amount of transpiration, evaporation, interception, and change in the soil water storage were quantified and modelled. As secondary soil climate modifier role CO<sub>2 emitting of different plant production forms and land-uses is shown. Estimated CO2 production burning fuels for soil and plant cultivation is one to threefold of the organic extensive and intensive plant production farm consecutively in 2001. For the estimative calculations cost data of the farms are used. Amount of CO<sub>2</sub> fixed in the crop biomass is also one to threefold as estimated with the regional scale formula of CEEMA (Canadian Economic and Emission Model for Agriculture). Two secondary soil modifier examples of soil texture and land use pattern’s influence on local weather phenomena and near surface atmospheric processes as storm move and development are presented yet. Both studies demonstrate the significance of site-specific soil hydraulic parameters – as field capacity, usable and actual water storage – in formation of the local weather through the soil evaporation and plant transpiration in modelling studies. Of course variety of soil’s role is much wider as the examples show and even it is not known completely at present. Soil’s role in bioclimatology as new discipline will expectably be formulated in the future.
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14

del-Arco, Marcelino J., Octavio Rodríguez-Delgado, Juan R. Acebes, Antonio García-Gallo, Pedro L. Pérez-de-Paz, Juana M. González-Mancebo, Ricardo González-González, and Víctor Garzón-Machado. "Bioclimatology and Climatophilous Vegetation of Gomera (Canary Islands)." Annales Botanici Fennici 46, no. 3 (June 2009): 161–91. http://dx.doi.org/10.5735/085.046.0301.

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15

Jendritzky, G. "Selected questions of topical interest in human bioclimatology." International Journal of Biometeorology 35, no. 3 (1991): 139–50. http://dx.doi.org/10.1007/bf01049060.

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16

MAHMOUDI, PEYMAN, SAFDAR ALI SHIRAZI, SEYED MAHDI AMIR JAHANSHAHI, FATEMEH FIROOZI, and NAUSHEEN MAZHAR. "A satellite bioclimatology of Baluchistan in Southwestern Asia." MAUSAM 75, no. 1 (December 31, 2023): 73–88. http://dx.doi.org/10.54302/mausam.v75i1.3573.

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.The present study aimed at investigating the relationship between two variables of temperature and precipitation with vegetation dynamics in one of the arid and semi-arid regions of the world, i.e. Baluchistan in Southwestern Asia, which is shared by the three countries of Iran, Pakistan and Afghanistan. In order to achieve the objectives, two different databases were used: 1. MODIS NDVI 16-day composite products (MOD13A3) of Terra satellite, with 1*1 km spatial resolution, which was obtained for a 17-year period (2000-2016) from the Earth Observing System (EOS) Data Gateway of the National Aeronautics and Space Administration (NASA); 2. Gridded monthly temperature and precipitation data was obtained for the same 17-year period from the Climate Research Unit (CRU) of the University of East Anglia. The Pearson product-moment correlation coefficient was also used to examine the relationship between vegetation dynamics and two climate variables of temperature and precipitation simultaneously as well as in three time lags i.e.; one month, two months and three months. The results of the analysis of a correlation between the mean temperature and monthly NDVI in different time lags indicated that in the humid and semi-humid regions in the northern half of Baluchistan, NDVI simultaneously reacted to temperature variations, while in the arid and semi-arid regions in the southern half of Baluchistan, NDVI had a one-month time lag with temperature. However, the results of the analysis of a correlation between precipitation and monthly NDVI in different time lags indicated that NDVI simultaneously reacted to precipitation variations, that is precipitation of each month had the greatest effect on the NDVI of the same month.
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17

Dotsenko, E. A., T. Y. Krestyaninova, and E. P. Bobrova. "INFLUENCE OF WEATHER-CLIMATIC CONDITIONS ON BRONCHIAL ASTHMA COURSE (LITERATURE REVIEW)." Health and Ecology Issues 1, no. 2 (February 15, 2004): 41–48. http://dx.doi.org/10.51523/2708-6011.2004-1-2-7.

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There is a review of investigations in the area of bioclimatology. It is described basic pathophysiological and clinical results, concerning of the weather's influence to the bronchial asthma. Our data prove that the high atmospheric pressure, high humidity and temperature gradient are reason of asthma attack. This results can be use for determination of optimal «asthma behaviour».
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18

Antonescu, Bogdan, Luminiţa Mărmureanu, Jeni Vasilescu, Cristina Marin, Simona Andrei, Mihai Boldeanu, Dragoş Ene, and Alexandru Ţilea. "A 41‐year bioclimatology of thermal stress in Europe." International Journal of Climatology 41, no. 7 (February 28, 2021): 3934–52. http://dx.doi.org/10.1002/joc.7051.

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19

Bazan, Giuseppe, Pasquale Marino, Riccardo Guarino, Gianniantonio Domina, and Rosario Schicchi. "Bioclimatology and Vegetation Series in Sicily: A Geostatistical Approach." Annales Botanici Fennici 52, no. 1-2 (April 2015): 1–18. http://dx.doi.org/10.5735/085.052.0202.

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20

Abels, David J., and Vitaly Kipnis. "Bioclimatology and balneology in dermatology: a Dead Sea perspective." Clinics in Dermatology 16, no. 6 (November 1998): 695–98. http://dx.doi.org/10.1016/s0738-081x(98)00059-5.

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21

Harlfinger, Otmar. "Holiday bioclimatology: a study of Palma de Majorca, Spain." GeoJournal 25, no. 4 (December 1991): 377–81. http://dx.doi.org/10.1007/bf02439488.

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22

Briccoli Bati, C., B. Filippucci, and D. Monardo. "BIOCLIMATOLOGY OF OLIVE: EFFECTS OF CLIMATIC CONDITIONS ON FLOWER BIOLOGY." Acta Horticulturae, no. 586 (October 2002): 493–96. http://dx.doi.org/10.17660/actahortic.2002.586.102.

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23

Del-Arco, M., J. R. Acebes, and P. L. Perez-de-Paz. "Bioclimatology and climatophilous vegetation of the Island of Hierro (Canary Islands)." Phytocoenologia 26, no. 4 (December 1, 1996): 445–79. http://dx.doi.org/10.1127/phyto/26/1996/445.

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24

Gopar-Merino, Fernando, Alejandro Velazquez, Alejandro González-Pérez, Sara del Río, Jean F. Mas, and Ángel Penas. "A coupled cartographic approach between bioclimatology and vegetation formations of Mexico." Vegetation Classification and Survey 5 (July 3, 2024): 153–64. http://dx.doi.org/10.3897/vcs.120442.

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Aims: The task of classifying and naming Mexican vegetation types has been undertaken by previous botanists, ecologists, and mapping agencies. However, discrepancies remain due to the lack of criteria and joint efforts from a geographical and botanical perspective. We aim to unravel the complex interactions between climate and vegetation in Mexico using climatic data and advanced mapping techniques, display in maps the transition from land cover to vegetation maps and couple geobotanical and bioclimatological approaches to provide a sound, unified system for identifying Mexican bioclimatic physiognomic patterns. Methods: Bioclimatic mapping was developed from the Digital Climatic Atlas of Mexico data source. In addition, land cover and vegetation data were obtained from the National Institute of Statistics and Geography of Mexico regrouped as described by the Standardized Hierarchical Vegetation Classification. These data were analysed via standard map crossing technics using geographic information systems. Results and conclusions: The results revealed five ombrotypes and five thermotypes, leading to the identification of 13 different bioclimatic classes, which, when combined with physiognomic types, led us to recognize 11 forests, 3 shrublands and 3 herbaceous formations (at a scale of 1:4,000,000). The core outcome is a detailed bioclimatic/physiognomic vegetation map including forests, shrublands and areas dominated by Herbaceous/Non-Vascular formations. The map highlights the critical importance of harmonising methodologies to ensure comprehensive and accurate insights into Mexico’s bioclimatic diversity. Taxonomic reference: Villaseñor et al. (2005). Syntaxonomic reference: Velázquez et al. (2021). Abbreviations: INEGI = Instituto Nacional de Estadística y Geografía; SECLAVEMEX = Standardized Hierarchical Vegetation Classification; WBCS = Worldwide Bioclimatic Classification System.
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25

Del-Arco, Marcelino, Juan-Ramón Acebes, Pedro-Luis Pérez-de-Paz, and María del Carmen Marrero. "Bioclimatology and climatophilous vegetation of Hierro (part 2) and La Palma (Canary Islands)." Phytocoenologia 29, no. 2 (June 23, 1999): 253–90. http://dx.doi.org/10.1127/phyto/29/1999/253.

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26

Barber, Antoni, Juan Tun, and Manuel B. Crespo. "A new approach on the bioclimatology and potential vegetation of the Yucatan Peninsula (Mexico)." Phytocoenologia 31, no. 1 (March 23, 2001): 1–31. http://dx.doi.org/10.1127/phyto/31/2001/1.

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27

Cano-Ortiz, Ana, Jose Carlos Piñar Fuentes, Felipe Leiva Gea, Jehad Mahmoud Hussein Ighbareyeh, Ricardo Jorje Quinto Canas, Catarina Isabel Rodrigues Meireles, Mauro Raposo, et al. "Climatology, Bioclimatology and Vegetation Cover: Tools to Mitigate Climate Change in Olive Groves." Agronomy 12, no. 11 (November 1, 2022): 2707. http://dx.doi.org/10.3390/agronomy12112707.

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This work establishes the relationship between bioclimatology and agronomy. Bioclimatic indices are obtained for several areas under olive cultivation and correlated with olive yields. Due to the effect of climate change on cultivation and the high economic losses it produces, we propose a sustainable development model for the territorial classification of crops based on bioclimatic knowledge. Bioclimatic diagrams are prepared to provide information on water stress in crops so that irrigation can be carried out at the most effective time, a measure that has been shown to lead to water and energy savings for growers. In addition to this development model, we propose the application of non-aggressive cultivation techniques such as the use of living plant cover to ensure the protection of the soil and avoid losses due to climate irregularities. Studies conducted up to the present on applied bioclimatology have yielded promising results in the fields of farming and forestry. The maps and bioclimatic indices of Professor Rivas-Martínez, Ic, Io and It/Itc, are essential for bioclimatic classification. The agricultural development model with a bioclimatic basis ensures economic savings for growers and minimizes the environmental impact of cultivation. In the case of olive cultivation we detected that in 2005 all the cultivated areas that were not in their thermoclimatic optimum were damaged by frost. The widespread cultivation of olive groves in the Mediterranean basin, and mainly in the south of Spain, is reason enough to establish a relationship between its production and its bioclimatic environment. The ombroclimatic study in certain localities under olive cultivation shows that areas with Io <2.5 are unproductive (Jodar, Tabernas), and that their low Io value needs to be supplemented with irrigation water. This means extracting water from aquifers for agricultural use, when the current climate irregularities do not allow the excessive use of subsoil water. For the time being the only way of mitigating this situation is with sustainable development, which requires a bioclimatic understanding of the territory; and the use of appropriate cultivation techniques, including herbaceous plant covers. In this last case a knowledge of the plant associations in the phytosociological class Stellarietea mediae constitutes the basis for establishing either natural or sown vegetation cover.
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28

Booth, Trevor H. "Perspective: Home and Away: The bioclimatology of Acacia species in Australia and overseas." Forest Ecology and Management 565 (August 2024): 122042. http://dx.doi.org/10.1016/j.foreco.2024.122042.

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29

Sevegnani, Kelly Botigeli, Silvia Helena Modenese-Gorla da Silva, Danielle Priscila Bueno Fernandes, and Iran José Oliveira Da Silva. "ESTUDO DA INFLUÊNCIA DE FATORES AMBIENTAIS EM VARIÁVEIS FISIOLÓGICAS DE FRANGOS DE CORTE COM REDES NEURAIS ARTIFICIAIS." ENERGIA NA AGRICULTURA 32, no. 2 (November 27, 2017): 148. http://dx.doi.org/10.17224/energagric.2017v32n2p148-152.

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Este trabalho investiga o uso de Redes Neurais Artificiais (RNAs) na análise da influência de fatores ambientais em diversos parâmetros fisiológicos em frangos de corte. Os dados deste trabalho foram obtidos em câmara climática do Núcleo de Pesquisa em Ambiência - NUPEA/ESALQ/USP. Machos e fêmeas de frangos de corte da linhagem Ross com 21, 28, 35, 42 e 49 dias de idade foram submetidos a quatro combinações de temperatura e umidade relativas. As RNAs foram utilizadas para avaliação da influência e relação de variáveis tais como temperatura, umidade relativa, frequência respiratória, temperatura retal, idade, ganho de peso, tempo de permanência no comedouro e tempo de permanência no bebedouro. Os resultados mostraram que é difícil predizer a condição ambiental a qual o animal foi submetido pelo conjunto de dados. O menor erro foi obtido com a variável ganho de peso como saída, sugerindo que esta seja a mais fortemente correlacionada com as outras variáveis.PALAVRAS-CHAVE: Redes Neurais Artificiais, avicultura, ambiência. STUDY OF THE INFLUENCE OF ENVIRONMENTAL FACTORS IN BROILER USING ARTIFICIAL NEURAL NETWORKSABSTRACT: This work investigates the use of Artificial Neural Networks to analyse the influence of ambiental variables in broilers. Data was obtained in the climatic chamber of Nucleous of Bioclimatology Research (NUPEA/ESALQ/USP). Broilers (males and females) of Ross genetic with 21, 28, 35, 42 e 49 day-old were submited to four combinations of temperature and relative humidity. Artificial Neural Networks were applied to evaluation of the influence and correlation of variables such as temperature, relative humidity, respiratory frequency, retal temperature and age in the weight gain of broilers. The results showed that it is difficult to predict the environmental conditions that the animal was subjected by the data set. The smallest error was obtained with the variable weight gain as output, suggesting that this one is the most strongly correlated with the other variables. KEYWORDS: Artificial Neural Networks, poultry production, bioclimatology.
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30

Huu Xuan, Nguyen, Nguyen Khanh Van, Hoang Thi Kieu Oanh, and Vuong Van Vu. "THE CREATION OF BIOCLIMATIC VEGETATION MAP TO DEVELOP SUSTAINABLE AGRO FORESTRY IN BA AND KONE RIVER BASIN, VIETNAM." Ukrainian Geographical Journal, no. 1 (2021): 54–62. http://dx.doi.org/10.15407/ugz2021.01.054.

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Bioclimate and natural vegetation have a long - term relationship that identify the potential vegetation distribution at different areas. For that reason, bioclimatic classification system was applied to the territory of Ba and Kone river basin, Vietnam. The precipitation and temperature dataset of Ba and Kone river basin was collected from 17 climate, hydrology, rain gauge stations which allowed to create a bioclimatic map at a scale of 1:250.000. Three bioclimatic factors of thermal-moisture basic conditions such as annual temperature (TN), annual rainfall (RN), length of dry season (n) are selected as criteria system of Ba and Kone river basin’s bioclimate. In order to describe the relationships between bioclimatic variables and zonal vegetation units, the resulting map presented 12 bioclimatic units corresponding distribution of vegetation from low to high altitudes. By building bioclimatology map in Ba and Kone river basin, the government can develop sustainable agro forestry in Central Highlands and South Central Coast of Vietnam.
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31

Norooz Valashedi, Reza, and Hadigheh Bahrami Pichaghchi. "Investigation of Bioclimatology Factors on Prediction of Honeybee Performance in Climate Change Conditions (Case Study: Shahindej)." Research on Animal Production 10, no. 25 (November 1, 2019): 120–28. http://dx.doi.org/10.29252/rap.10.25.120.

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32

Idso, Sherwood B. "Advances in Bioclimatology. Volume 1.R. L. Desjardins , R. M. Gifford , T. Nilson , E. A. N. Greenwood." Quarterly Review of Biology 68, no. 1 (March 1993): 130. http://dx.doi.org/10.1086/417989.

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33

Rispail, Philippe, Jacques Dereure, and Daniel Jarry. "Risk Zones of Human Leishmaniases in the Western Mediterranean Basin: Correlations between Vector Sand Flies, Bioclimatology and Phytosociology." Memórias do Instituto Oswaldo Cruz 97, no. 4 (June 2002): 477–83. http://dx.doi.org/10.1590/s0074-02762002000400004.

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34

Alonso-Pérez, Silvia, Javier López-Solano, Lourdes Rodríguez-Mayor, and José Miguel Márquez-Martinón. "Evaluation of the Tourism Climate Index in the Canary Islands." Sustainability 13, no. 13 (June 23, 2021): 7042. http://dx.doi.org/10.3390/su13137042.

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In this study, we performed a diagnostic and evolutive analysis of the bioclimatology of the Canary Islands, an Atlantic archipelago where the climate itself is a main feature promoting tourism. Among all the tourist-climate indices described in the literature, we evaluated the most widely used, which is the Tourism Climate Index (TCI) proposed by Mieczkowski (1985). Monthly mean TCI time series were calculated using meteorological data from the Spanish State Meteorological Agency database and the European Climate Assessment and Dataset. Our results show TCI values greater than 50 during almost every month in the period 1950–2018, with mean values over the entire time series between 70 and 80. According to the TCI classification scheme, these values correspond to a very good thermal comfort along all of the period. Our results also point to spring as the season with the best TCI, with maximum values around 80 for this index in April—excellent according to the TCI classification. However, we did not find a correlation between inbound arrivals and the TCI index, which might point to a lack of information available to tourists. This opens an opportunity for policymakers and tour operators to better publicize the best seasons for holidays in the islands.
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Milentijevic, Nikola, Jovan Dragojlovic, Marija Cimbaljevic, Dusan Ristic, Kristina Kalkan, and Dragan Buric. "Analysis of equivalent temperature - case of Kragujevac city." Glasnik Srpskog geografskog drustva 98, no. 1 (2018): 61–77. http://dx.doi.org/10.2298/gsgd180225003m.

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A more complete climate image of a site is obtained by analyzing bioclimatic indicators. In this paper, an analysis of the physiological sense of heat in the territory of the city of Kragujevac was presented. Bioclimatic considerations are based on the equivalent temperature, which represents the combined influence of air temperature and water vapor pressure. Based on these two climatic elements, the corresponding equations and the Kr?ger anthropo-climatic classifications, three climate types and nine physiological sensations of heat for the territory of the city of Kragujevac were isolated. Their significance in bioclimatology is that they cause different sensations of heat in healthy and sick people, and can serve as the basis for the expected types of bioclimate during the year. Urban areas are areas of higher population concentration to which the climate elements act stimulating or, on the contrary, discouraging, which depends on the person's health. For the needs of this work, a thirty-year climate period (1981-2010) was analyzed based on the data obtained from the weather station Kragujevac. There are significant historical and tourist sites and natural resources in the city and its surroundings, which can be valorized complementarily. Analyzed values of equivalent temperatures can be used for the planning of tourist activities and in means of tourist propaganda. For this purpose, this work can be a solid bioclimatic basis.
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36

Bustamante Oleart, Carlos. "La historia del viento en las ciudades = The history of the wind in the cities." Cuadernos de Investigación Urbanística, no. 132 (October 30, 2020): 1. http://dx.doi.org/10.20868/ciur.2020.132.4510.

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ResumenLa relación entre el viento y las ciudades se desarrolla a lo largo de la historia de manera accidentada, discontinua y en varias disciplinas. En sus orígenes, el conocimiento del viento era más de carácter intuitivo y se basaba en la observación de sus manifestaciones visibles, ya sea en la lluvia, los remolinos o los elementos que arrastra. Estas observaciones permitieron, en diversa épocas, generar ciertos criterios para diseñar ciudades con principios eólicos genéricos. Con el paso del tiempo, los avances científicos y las nuevas tecnologías, fue posible ir avanzado en el conocimiento del viento. Así, diversas disciplinas como la geografía, la meteorología, la arquitectura y el urbanismo avanzaron por caminos separados, cada una buscando sus propios objetivos en relación al viento. A medida que nos acercamos al siglo XX empiezan a aparecer ramas de estas mismas disciplinas, como la climatología o la bioclimatología, sumándose también nuevas áreas del conocimiento como la ingeniería aeroespacial, la que se desprende la ingeniería aerodinámica para cuerpos romos no fuselados y cuerpos estáticos como los edificios, los puentes, etc. Todas estas ramas del conocimiento desarrollan caminos paralelos, pero al final del siglo XX y comienzos del XXI se empiezan a mezclar, compartiendo sus propios descubrimientos. Hoy, la necesidad de reunir estos conocimientos se torna fundamental para lograr un avance interdisciplinario que permita comprender la importancia del viento para la planificación urbana en un mundo que necesita cada vez más conciencia ambiental.AbstractThe relationship between the wind and the cities has developed throughout history in an uneven, discontinuous way and in various disciplines. In its origins, the knowledge of the wind was more intuitive in nature and was based on the observation of its visible manifestations, whether in the rain, the eddies or the elements that it drags. These observations allowed, at different times, to generate certain criteria to design cities with generic wind principles. With the passage of time, scientific advances and new technologies, it was possible to advance in the knowledge of the wind. Thus, various disciplines such as geography, meteorology, architecture and urban planning advanced in their separate ways, each seeking its own objectives in relation to the wind. As we approach the 20th century, branches of these same disciplines begin to appear, such as climatology or bioclimatology, also adding new areas of knowledge such as aerospace engineering, which is derived from aerodynamic engineering for non-fuselated blunt bodies and static bodies. like buildings, bridges, etc. All these branches of knowledge develop parallel paths, but at the end of the 20th century and the beginning of the 21st they begin to mix, sharing their own discoveries. Today, the need to gather this knowledge becomes fundamental to achieve an interdisciplinary advance that allows understanding the importance of the wind for urban planning in a world that increasingly needs environmental awareness.
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Di Filippo, Alfredo, Franco Biondi, Katarina Čufar, Martín de Luis, Michael Grabner, Maurizio Maugeri, Emanuele Presutti Saba, Bartolomeo Schirone, and Gianluca Piovesan. "Bioclimatology of beech (Fagus sylvatica L.) in the Eastern Alps: spatial and altitudinal climatic signals identified through a tree-ring network." Journal of Biogeography 34, no. 11 (November 2007): 1873–92. http://dx.doi.org/10.1111/j.1365-2699.2007.01747.x.

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Tan, S. ‐Y. "The influence of temperature and precipitation climate regimes on vegetation dynamics in the US Great Plains: a satellite bioclimatology case study." International Journal of Remote Sensing 28, no. 22 (October 23, 2007): 4947–66. http://dx.doi.org/10.1080/01431160701264268.

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Pecelj, Milica, Aleksandar Djordjevic, Milovan Pecelj, Jelena Pecelj-Purkovic, Dejan Filipovic, and Velimir Secerov. "Biothermal conditions on Mt. Zlatibor based on thermophysiological indices." Archives of Biological Sciences 69, no. 3 (2017): 455–61. http://dx.doi.org/10.2298/abs151223120p.

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This paper presents part of the research in the field of human bioclimatology and refers to biothermal conditions in different geographical environments in Serbia: an urban area and a mountain of medium height. The goal of the paper was to show bioclimatic differences during the summer between the city of Belgrade (116 m a.s.l.) and the mountain resort of Zlatibor (1498 m a.s.l.). The basic principle of bioclimatic analysis is the human heat balance between man and environment. This methodological approach is a combination of physiological and meteorological parameters that result in thermophysiological bioclimatic indices: heat load (HL) in man and the Universal Thermal Climate Index (UTCI). For this analysis, weather data for July, as the warmest month, was obtained, using daily meteorological data for the decade from 2000 to 2010. Results for July indicate a considerable difference between the two abovementioned environments. HL in Belgrade was dominated by degrees of comfort ?hot? and ?extremely hot, with the highest value of 4.540, while for Zlatibor the dominant degree of comfort was ?warm?. The UTCI in Belgrade has dominated by strong heat stress and moderate heat stress, compared to Zlatibor where the UTCI is dominated by moderate heat stress. In addition, a significant part of the monitored decade on Mt. Zlatibor was without heat stress, with the exception of 2006 and 2007, indicating favorable biothermal characteristics. Therefore, compared to Belgrade, with its considerably lower overall heat stress Zlatibor has the characteristics of a site with favorable bioclimatic qualities.
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Bouzahar, Chafika, Yamina Kadid, Badia Siab-Farsi, Frédéric Bioret, Yacine Boulenouar, and Zoubir Boubaker. "Bioclimatologie et syntaxonomie des forêts de chêne vert (Quercus rotundifoliaLam.) du Dahra oriental dans la région de Tipaza (Algérie) / Bioclimatology and syntaxonomy of the Holm Oak forests (Quercus rotundifolia Lam.) of eastern Dahra in the Tipaza region (Algeria)." Ecologia mediterranea 47, no. 2 (2021): 5–26. http://dx.doi.org/10.3406/ecmed.2021.2127.

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Yarmishko, V. T., O. V. Ignatieva, and F. A. Chepik. "HISTORICAL DEVELOPMENT OF BOTANY AS A FOUNDATION FOREST EDUCATION AND SCIENCE IN RUSSIA." ÈKOBIOTEH 3, no. 3 (2020): 379–89. http://dx.doi.org/10.31163/2618-964x-2020-3-3-379-389.

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The Department of Botany and Dendrology of the oldest educational forestry institution of Russia, the present St. Petersburg State Forest Technical University named after S.M. Kirov, is celebrating its centenary. At the time of its foundation it was the first specialized department of this kind both in Russia and in the world. In the course of its historical development, the Department of Botany and Dendrology has been formed not only as a large educational and methodological center for botanical, dendrological and general biology training. It has also become a major scientific center providing a wide range of research in the field of biology and ecology of woody plants, their introduction, intraspecific polymorphism, selection, phenological biorhythm, forest science, floristics and taxonomy, anthropogenic dynamics of plant cover and biodiversity conservation of forest ecosystems, bioindication, bioclimatology, forest phenology, and dendrophenological forecasting. It is impossible to list scientific publications of the Department, for only V.N.Sukachov alone was the author of about 500 papers. Under the leadership of V.N.Sukachev, his students and followers, provided research training and supervision for about 50 doctors and candidates of sciences, most of whom specialized in dendrology. Already in itself this fact testifies that creating the first in Russia Department of dendrology, V.N.Sukachev looked far ahead into addressing botanical and dendrological problems of Russia. Only within the last 10-15 years, the staff of the Department published 10 monographs, 2 textbooks, more than 10 teaching manuals. The geography of scientific research is constantly expanding. The scientific school “Dendrology and Biogeocenology named after V.N.Sukachev” has been established and is functioning at the Department.
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González-Pérez, Alejandro, Ramón Álvarez-Esteban, Ángel Penas, and Sara del Río. "Bioclimatic Characterisation of Specific Native Californian Pinales and Their Future Suitability under Climate Change." Plants 12, no. 10 (May 12, 2023): 1966. http://dx.doi.org/10.3390/plants12101966.

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Rising temperatures and changes in precipitation patterns under climate change scenarios are accelerating the depletion of soil moisture and increasing the risk of drought, disrupting the conditions that many plant species need to survive. This study aims to establish the bioclimatic characterisation, both qualitative and quantitative, of ten native Californian Pinales for the period 1980–2019, and to determine their habitat suitability by 2050. To achieve this, an exhaustive search of the Gbif database for records of ten conifer taxa was carried out. To conduct the bioclimatic characterisation of the studied taxa, we worked with the monthly values of average temperature and precipitation for the period 1980–2019 from 177 meteorological stations. Linear regressions was performed in order to compile the future evolution of California’s climate. Suitable areas and optimal areas were defined at the present time (1980–2019) and its future projection (2050). We applied Boolean logic and, in this investigation, the Conditional Logic Operator (CON) was used to determine the possible species presence (one) or absence (zero) for each of the 15 variables analysed. In general, most of the conifers studied here will experience a reduction in their habitat range in California by the year 2050 due to climate change, as well as the displacement of species towards optimal areas. Furthermore, the results have highlighted the applicability of bioclimatology to future conditions under climate change. This will aid conservation managers in implementing strategic measures to ameliorate the detrimental impacts of climate change, thereby ensuring the ecological integrity and sustainability of the affected conifer species.
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Kipriyanova, L. M., Yu V. Plugatar, N. V. Matveyeva, and N. B. Ermakov. "Scientific workshop «Theoretical problems of the classification of the plant communities of Russia» (Yalta, November 1–3, 2021)." Vegetation of Russia, no. 42 (2021): 165–68. http://dx.doi.org/10.31111/vegrus/2021.42.165.

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Thirty years after the publication of the USSR vegetation syntaxa prodromus (Korotkov et al., 1991), the active work on the preparation of the Prodromus of the Russian Federation vegetation (Plugatar et al., 2020) has started. 29 contributions (incl. 5 via Skype), were represented at the Workshop “Theoretical problems of the classification of plant communities of Russia”, that took place in Yalta, Republic of Crimea, on November 1–3, 2021. Twenty six scientists (Fig. 1, 2) from St. Petersburg, Moscow, Novosibirsk, Ufa, Vladivostok, Yakutsk, Syktyvkar, Bryansk, Rostov on Don, Khanty-Mansiysk, Ekaterinburg, Nalchik, Kursk, Yalta) participated this meeting. The reviews of syntaxonomic systems of forests, steppes, meadows, and aquatic, halophytic, synantropic, alpine, arctic, petrophytic, see-shore vegetation and wetlands were represented. The problems, that have appeared after beginning the syntaxa checklists development, such as the validation of units, the dubiousness of some accepted syntaxonomic decisions, poor syntaxonomic knowledge of some regions were discussed. The directors of three Botanical Gardens (from Yalta, Novosibirsk and Vladivostok) of the Russian Academy of Sciences signed documents (Fig. 3) on the starting of a scientific consortium «National Network of Botanical Gardens of the Russian Federation», focused on joint fundamental researches in the vegetation science, ecology, bioclimatology and biogeography; on the development of the National classification of vegetation and National typology of habitats as a scientific basis for assessing the carbon balance, rational use of natural resources and vegetation conservation in the country. Resolution of the Workshop emphasizes the necessity to consider the development of the Russian national vegetation classification as a priority task for phytosociologists in Russian Federation for the next five years.
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Ramaswamy, S. S. "Physiological Research of Defence Interest in India Part II: Studies in Thermal Stress Noise Exposure Hazards Bioclimatology Physical Work Capacity and Effects of Ageing." Defence Science Journal 44, no. 3 (January 1, 1994): 241–49. http://dx.doi.org/10.14429/dsj.44.4176.

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Le Houerou, Henry Noel. "Bioclimatology and Phytogeography of the Red Sea and Aden Gulf Basins: A Monograph (with a Particular Reference to the Highland Evergreen Sclerophylls and Lowland Halophytes)." Arid Land Research and Management 17, no. 3 (January 2003): 177–256. http://dx.doi.org/10.1080/15324980301601.

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Antoniadis, Dimitrios, Nikolaos Katsoulas, and Dimitris Κ. Papanastasiou. "Thermal Environment of Urban Schoolyards: Current and Future Design with Respect to Children’s Thermal Comfort." Atmosphere 11, no. 11 (October 22, 2020): 1144. http://dx.doi.org/10.3390/atmos11111144.

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Urban outdoor thermal conditions, and its impacts on the health and well-being for the city inhabitants have reached increased attention among biometeorological studies during the last two decades. Children are considered more sensitive and vulnerable to hot ambient conditions compared to adults, and are affected strongly by their thermal environment. One of the urban outdoor environments that children spend almost one third of their school time is the schoolyard. The aims of the present manuscript were to review studies conducted worldwide, in order to present the biophysical characteristics of the typical design of the urban schoolyard. This was done to assess, in terms of bioclimatology, the interactions between the thermal environment and the children’s body, to discuss the adverse effects of thermal environment on children, especially the case of heat stress, and to propose measures that could be applied to improve the thermal environment of schoolyards, focusing on vegetation. Human thermal comfort monitoring tools are mainly developed for adults, thus, further research is needed to adapt them to children. The schemes that are usually followed to design urban schoolyards create conditions that favour the exposure of children to excessive heat, inducing high health risks to them. The literature survey showed that typical urban schoolyard design (i.e., dense surface materials, absence of trees) triggered high surface temperatures (that may exceed 58 °C) and increased absorption of radiative heat load (that may exceed 64 °C in terms of Mean Radiant Temperature) during a clear day with intense solar radiation. Furthermore, vegetation cover has a positive impact on schoolyard’s microclimate, by improving thermal comfort and reducing heat stress perception of children. Design options for urban schoolyards and strategies that can mitigate the adverse effects of heat stress are proposed with focus on vegetation cover that affect positively their thermal environment and improve their aesthetic and functionality.
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Pohanková, Eva, Petr Hlavinka, Jozef Takáč, Zdeněk Žalud, and Miroslav Trnka. "Calibration and Validation of the Crop Growth Model DAISY for Spring Barley in the Czech Republic." Acta Universitatis Agriculturae et Silviculturae Mendelianae Brunensis 63, no. 4 (2015): 1177–86. http://dx.doi.org/10.11118/actaun201563041177.

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In this paper, the crop growth model DAISY for spring barley (cultivar “Tolar“) was calibrated and subsequently validated in three different soil-climate locations in the Czech Republic – Lednice (48°48'51'' N, 16°48'46'' E, altitude 180 m), Věrovany (49°27'39'' N, 17°17'42'' E, altitude 210 m) and Domanínek (49°31'42'' N, 16°14'13'' E, altitude 560 m). The calibration and validation were based on data from a multi-year field experiment from the Central Institute for Supervising and Testing in Agriculture and from a two-year field experiment in Domanínek (2011 and 2012) that was conducted by the Institute of Agrosystems and Bioclimatology in cooperation with the Global Change Research Centre AS CR. The calibration for Lednice, Věrovany and Domanínek was performed using 4 growth seasons from each station, the subsequent validation for Lednice and Věrovany was performed based on 3 growth seasons from each station, and that for Domanínek was based on 6 growth seasons. The value of the RMSE (root mean square error) statistic for flowering was 2 days for calibration and 4 days for validation on average; for maturity, the RMSE was 11 days for both calibration and validation. The average RMSE for the yields was 0.9 t·ha−1 for calibration and 1.6 t·ha−1 for validation. According to the statistical index MBE (mean bias error) for the flowering phenological phase, the crop growth model DAISY showed a delay of 2 days in both calibration and validation. There was also delay of 6 days in calibration and of 8 days in validation for maturity. According to the MBE, the crop growth model DAISY underestimates the yield by 0.2 t·ha−1 for calibration and underestimates the yield by 0.4 t·ha−1 for validation.
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Gianguzzi, Lorenzo, Riccardo Guarino, Giuseppe Bazan, Romeo Di Pietro, Alicia Teresa Rosario Acosta, Enrico Bajona, Peter Bolliger, et al. "Itineraries of the Working Group for Vegetation Science of the Italian Botanical Society – 1 (2022): Excursion to the Egadi Islands, Mount San Giuliano and Mount Cofano (Trapani, western Sicily, Italy)." Italian Botanist 16 (July 31, 2023): 1–57. http://dx.doi.org/10.3897/italianbotanist.16.103989.

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The results of the annual excursion of the Working Group for Vegetation Science of the Italian Botanical Society, held in the Egadi Islands, Mount San Giuliano and Mount Cofano (W Sicily) on April 23–27 2022, are presented. This paper includes: (1) general information on the visited sites; (2) geology and geomorphology; (3) climatology and bioclimatology with tables of climatic data; (4) description of the following five geobotanical itineraries – accompanied by 29 original vegetation relevés and 11 synthetic relevés, proceeding from different bibliographic references: (a) Mount San Giuliano; (b) Marettimo Island: coastal and sub-coastal stretch of the southern part, between Punta Bassana and Contrada Chiappera; (c) Marettimo Island: Case Romane, Mount Pizzo Falcone and the north-western coastal stretch; (d) Island of Levanzo; (e) Mount Cofano – with catenal pictograms of the vegetation, surveys and description of the plant communities and related syntaxonomic scheme; (5) list of the surveyed plant taxa, collected specimens and herbaria in which they are deposited. A new syntaxon is also described (Catapodio pauciflori-Moraeetum sisyrinchii ass. nova), referring to an ephemeral dry grassland located along the north-western coastal stretch of Marettimo. The new association is framed in the Plantagini-Catapodion balearici, alliance of the Stipo-Bupleuretalia semicompositi order of the class Stipo-Trachynietea distachyae (order Stipo-Bupleuretalia semicompositi, alliance Plantagini-Catapodion balearici). An original synoptic table, regarding 17 different plant communities with high frequency of Moraea sisyrinchium, provides a comparative framework of the new association with allied vegetation units so far described throughout the Mediterranean region. Syntaxonomical and nomenclatural remarks regarding the Mediterranean vegetation occurring in this territory are also given throughout the text. Some floristic updates for the study sites are also reported, including the discovery for the first time in Sicily of Lysimachia loeflingii.
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Maciołek, Ryszard. "KAZIMIERZ MARCINIAK'S VIEWS ON SCIENCE TASKS." Modern Higher Education Review, no. 6 (2021): 26–45. http://dx.doi.org/10.28925/2518-7635.2021.62.

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This article is devoted to the person and his views on the role of scientific activity in the life of the university and its significance for the social life. Kazimierz Marciniak represented geography and he specialized in climatology and bioclimatology. His extensive academic experience, gained through studies and scientific work at several Polish universities and in the Institute of Balneology in Poznań, made him not only an excellent researcher, but also a scholar whose views on the role of science in the life of the university and in social life were influencing the generation of representatives of many sciences who worked at the WSG University in Bydgoszcz. The convictions of the scholar in question, his broad vision of science not only as an enterprise calculated on commercial values, place him among the outstanding Polish scientists and philosophers. He shared with them not only the conviction about the cognitive function of science, which was engaged in economic activity, but also noticed its highly humanistic and ennobling role in relation to the researcher, in which the creative aspects of his work are present. Scientific work also contributes to the improvement of the educational process. Participation of a student, in any form of scientific activity, shapes his intellectual and even moral skills, educates in the spirit of the culture of the word, especially the written one. In the opinion of the discussed author, the main function of science for the entire social life is to forecast phenomena. Exploratory and exploratory functions are important, however, they are subordinated to the former. His methodological and philosophical views on the structure and dynamics of scientific theories were characterised by inductivism and probabilism. Some of his views on the questions of the nature of phenomena, the structure of reality and the relation between scientific theory and reality, were not presented in an unambiguous way; it also seems that they evolved towards anti-phenomenalism, anti-foundationalism and essentialism, which distanced him from scientism, as a worldview quite characteristic of representatives of the natural sciences of the 20th century.
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Matviienko, M. O. "ENVI-MET MODEL AS A TOOL FOR MODERN URBAN METEOROLOGICAL STUDIES." Hydrology, hydrochemistry and hydroecology, no. 4 (55) (2019): 151–63. http://dx.doi.org/10.17721/2306-5680.2019.4.13.

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Studying the microclimate of cities is one of the areas of urban meteorology, which are actively developing recently. The research of microclimate and its dependence on building parameters is important not only for scientists but also for architects, engineers and urban planners. Because they can help make the urban environment more comfortable for living and minimize the negative impact of Urban Heat Island, which is especially important in the context of rapid urbanization and in the face of climate change, that is most often reflected in air temperatures increasing. For modern urbanmeteorological studies traditional methods (observation method and statistical methods) cannot remain basic, so they are replaced by numerical simulation tools. One of those tools is the Computational Fluid Dynamics (CFD), which are based on the use of numerical methods to simulate the interaction between the atmosphere and the urban surface. Such approaches are gaining in popularity because of such advantages as accurate modeling of urban geometry and the high-resolution description of airflow in it; the ability to simulate the microclimate in different conditions (weather, buildings, vegetation, water bodies, etc.); numerical simulation can provide information about any researched variable in the entire simulated area. This article describes the modern ENVI-met microclimate model as one of the most common numerical simulation tools. The model is based on the fundamental laws of fluid dynamics and thermodynamics and is able to reproduce the basic processes of interaction between the atmosphere, soil, vegetation and buildings. The model can be used to simulate microclimate conditions, bioclimatology, urban air pollution, and to identify optimal measures for urban adaptation to climate change. The paper provides an overview of studies published in peer-reviewed international journals (in the period from 1999 to the end of 2018) using the ENVI-met model, and also presents its main advantages and disadvantages. The simulation accuracy of the ENVI-met model is analyzed by comparing the simulated data with the measured one.
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