Russian Journal of Earth Sciences Russian Journal of Earth Sciences Russian Journal of Earth Sciences 1681-1208 53402 10.2205/2022ES01SI04 СПЕЦВЫПУСК: "ФУНДАМЕНТАЛЬНЫЕ И ПРИКЛАДНЫЕ АСПЕКТЫ ГЕОЛОГИИ, ГЕОФИЗИКИ И ГЕОЭКОЛОГИИ" Special Issue: "Fundamental and applied aspects of geology, geophysics and geoecology" СПЕЦВЫПУСК: "ФУНДАМЕНТАЛЬНЫЕ И ПРИКЛАДНЫЕ АСПЕКТЫ ГЕОЛОГИИ, ГЕОФИЗИКИ И ГЕОЭКОЛОГИИ" Modern changes in the precipitation and air temperature regime in the mountainous regions of the Dagestan Republic Modern changes in the precipitation and air temperature regime in the mountainous regions of the Dagestan Republic https://orcid.org/0000-0001-9368-1666 Корчагина Елена Александровна Korchagina Elena Aleksandrovna ФНЦ "Кабардино-Балкарский научный центр РАН" Нальчик Россия Federal Scientific Center "Kabardino-Balkarian Scientific Center of the RAS" Nalchik Russian Federation 04 12 2022 04 12 2022 22 5 1 8 01 07 2022 10 08 2022 https://rjes.ru/en/nauka/article/53402/view

The study focuses on the local dynamics of precipitation and temperature in the mountainous regions of the Dagestan Republic (North Caucasus, eastern part). A shift in the secondary maximum of the precipitation annual distribution in the low-mountainous part of the region from August to September was found. The wettest years in the highlands in the periods 1966-1978 and 1996-2013 are discovered. The period from the beginning of the current century until now is identified as the wettest in the low-mountain zone. It was found that the trends of seasonal temperatures are positive. At the same time, the dynamics of spring temperatures remained insignificant in the low-mountain zone until 2010. It was revealed that the statistically reliable increase of temperature in February and March and unidirectional tendencies in the daily characteristics of precipitation is the local pattern of the climate change in this part of the North Caucasus. In this season the increase in the average and maximum daily precipitation intensity is reliable.

The study focuses on the local dynamics of precipitation and temperature in the mountainous regions of the Dagestan Republic (North Caucasus, eastern part). A shift in the secondary maximum of the precipitation annual distribution in the low-mountainous part of the region from August to September was found. The wettest years in the highlands in the periods 1966-1978 and 1996-2013 are discovered. The period from the beginning of the current century until now is identified as the wettest in the low-mountain zone. It was found that the trends of seasonal temperatures are positive. At the same time, the dynamics of spring temperatures remained insignificant in the low-mountain zone until 2010. It was revealed that the statistically reliable increase of temperature in February and March and unidirectional tendencies in the daily characteristics of precipitation is the local pattern of the climate change in this part of the North Caucasus. In this season the increase in the average and maximum daily precipitation intensity is reliable.

 precipitation dynamics air temperature trends North Caucasus East Caucasus climate change in mountainous areas natural hazard precipitation dynamics air temperature trends North Caucasus East Caucasus climate change in mountainous areas natural hazard

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