2017
DOI: 10.1007/s00484-017-1470-6
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A comparison of bioclimatic potential in two global regions during the late twentieth century and early twenty-first century

Abstract: Changes in the general circulation of the atmosphere have been taking place during the latter part of the twentieth century and the early part of the twenty-first century. In the Belgorod region of Southwest Russia, this has been manifested in the more frequent occurrence of stationary anticyclones, including those referred to as blocking anticyclones, especially during the summer season. Also, there has been a general increase in regional temperatures during the growing season over the period mentioned above,… Show more

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Cited by 4 publications
(27 citation statements)
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“…In addition to the BCP, the moisture index in [17] was also calculated. Reference [14] used both of these quantities to study and compare yield potential for the central United States and southwest Russia. Additional material used in this research was the catalog of Northern Hemisphere (NH) circulation regime classifications (called essential circulation mechanisms or modes-ECM) as proposed by [18] in 1946 and used widely in later studies (e.g., [17,19,20]) and discussed in detail by [20][21][22].…”
Section: Methodsmentioning
confidence: 99%
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“…In addition to the BCP, the moisture index in [17] was also calculated. Reference [14] used both of these quantities to study and compare yield potential for the central United States and southwest Russia. Additional material used in this research was the catalog of Northern Hemisphere (NH) circulation regime classifications (called essential circulation mechanisms or modes-ECM) as proposed by [18] in 1946 and used widely in later studies (e.g., [17,19,20]) and discussed in detail by [20][21][22].…”
Section: Methodsmentioning
confidence: 99%
“…The Hydrothermal Coefficient (HTC) is also an indicator of moisture content published by the Soviet climatologist G. T. Selyaninov [23]. The HTC is determined by the ratio of the precipitation amount (r) (mm) during the period with average daily air temperatures above 10 • C to the sum of temperature ( T*) during the same time-period (multiplied by 0.1), that is: The HTC is one of the indicators of agricultural growth in different parts of the world (e.g., [14] and [24][25][26]). As an important agro-climatic indicator that defines the resource and energy demands of crops, the period when the daily mean temperature greater than 10°C is a viable baseline because it describes the period of active vegetation for a majority of plants, including sugar beets.…”
Section: Methodsmentioning
confidence: 99%
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