{"id":4041,"date":"2021-02-23T14:30:27","date_gmt":"2021-02-23T13:30:27","guid":{"rendered":"https:\/\/us.edu.pl\/instytut\/inoz\/?p=4041"},"modified":"2021-03-15T11:59:44","modified_gmt":"2021-03-15T10:59:44","slug":"rezim-lodowy-zbiornika-kozlowa-wskaznikiem-zmian-termicznych-otoczenia","status":"publish","type":"post","link":"https:\/\/us.edu.pl\/instytut\/inoz\/en\/2021\/02\/23\/rezim-lodowy-zbiornika-kozlowa-wskaznikiem-zmian-termicznych-otoczenia\/","title":{"rendered":"Ice Regime of the Koz\u0142owa G\u00f3ra Reservoir as an Indicator of Changes of the Thermal Conditions of Ambient Air"},"content":{"rendered":"
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The Hydrology and Water Use research team members published an article in the Water journal entitled \u2018Ice Regime of the Koz\u0142owa G\u00f3ra Reservoir (Southern Poland) as an Indicator of Changes of the Thermal Conditions of Ambient Air\u2019.<\/p>\n
Measurements and observations of ice phenomena in the Koz\u0142owa G\u00f3ra reservoir have been carried out since 1964. In 1964-2015, there was a decrease in the number of days with an ice cover (by 8.6 days per decade) and a decrease in the maximum and average thickness of lake ice (by 2.0 cm and 1.2 cm per decade, respectively). The small average depth and capacity of the reservoir are reflected in the rapid freezing rate of the reservoir, and the location results in a longer time of ice cover and greater thickness and later dates of ice melting, in relation to lakes located in northern Poland.<\/p>\n
Solarski, M.; Rz\u0119ta\u0142a, M. Ice Regime of the Koz\u0142owa G\u00f3ra Reservoir (Southern Poland) as an Indicator of Changes of the Thermal Conditions of Ambient Air. Water 2020, 12, 2435. https:\/\/doi.org\/10.3390\/w12092435<\/p>\n<\/div>\r\n <\/div>\r\n <\/div>[\/vc_column][vc_column width=”1\/2″][vc_single_image image=”4044″ img_size=”full”]\r\n
Fig.1<\/p>\n
Location of the Koz\u0142owa G\u00f3ra reservoir (A) together with its bathymetric plan (B): 1\u2014water courses and water reservoirs, 2\u2014major cities.<\/p>\n<\/div>\r\n <\/div>\r\n <\/div>[vc_single_image image=”4042″ img_size=”full”]\r\n
Fig 2.<\/p>\n
Changes in average air temperature in the winter half-year (XI\u2013IV) in the hydrological years 1964\u20132015 at the Katowice weather station and values of the winter NAODJFM index (D\u2014December, J\u2014January, F\u2014February, M\u2014March): 1\u2014NAODJFM index, 2\u2014average air temperature, 3\u2014average air temperature trend.<\/p>\n<\/div>\r\n <\/div>\r\n <\/div>[vc_single_image image=”4043″ img_size=”full”]\r\n
Fig. 5.<\/p>\n
RDA biplots illustrating relations between environmental variables and selected parameters of lake ice phenology for the Koz\u0142owa G\u00f3ra reservoir and lakes in northeastern Poland and northwestern Poland: 1\u2014correlated variables, 2\u2014lakes examined.<\/p>\n<\/div>\r\n <\/div>\r\n <\/div>[\/vc_column][\/vc_row]<\/p>","protected":false},"excerpt":{"rendered":"
[vc_row][vc_column width=”1\/2″][\/vc_column][vc_column width=”1\/2″][vc_single_image image=”4044″ img_size=”full”][vc_single_image image=”4042″ img_size=”full”][vc_single_image image=”4043″ img_size=”full”][\/vc_column][\/vc_row] […]<\/p>\n