Ice phenomena on Lake Czarny Staw pod Rysami
Due to its inaccessibility (in winter), Lake Czarny Staw pod Rysami (Black Lake below Mount Rysy) has no series of continuous observations concerning ice phenomena. For the purpose of supplementing knowledge in this scope, ice corings were performed in the years 2010–2015. They permitted the determi...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2016-03-01
|
| Series: | Limnological Review |
| Subjects: | |
| Online Access: | https://doi.org/10.1515/limre-2016-0018 |
| _version_ | 1797328150556835840 |
|---|---|
| author | Choiński Adam |
| author_facet | Choiński Adam |
| author_sort | Choiński Adam |
| collection | DOAJ |
| description | Due to its inaccessibility (in winter), Lake Czarny Staw pod Rysami (Black Lake below Mount Rysy) has no series of continuous observations concerning ice phenomena. For the purpose of supplementing knowledge in this scope, ice corings were performed in the years 2010–2015. They permitted the determination of the variability of ice cover thickness on the lake’s surface. A high degree of similarity was determined in the distribution of ice cover thickness in the analysed winters (in contrast to the nearby Lake Morskie Oko). Moreover, a correlation was determined according to which the thicker the snow cover overlying the ice, the thinner the ice cover. It was determined that the mean thickness of the ice cover of Lake Czarny Staw pod Rysami is higher by approximately a dozen cm than that on Lake Morskie Oko located around 200 m lower. |
| first_indexed | 2024-03-08T06:47:45Z |
| format | Article |
| id | doaj.art-fe6aa075890c4dada7f3187d8a4d6364 |
| institution | Directory Open Access Journal |
| issn | 2300-7575 |
| language | English |
| last_indexed | 2024-03-08T06:47:45Z |
| publishDate | 2016-03-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Limnological Review |
| spelling | doaj.art-fe6aa075890c4dada7f3187d8a4d63642024-02-03T07:34:15ZengMDPI AGLimnological Review2300-75752016-03-0116316516910.1515/limre-2016-0018limre-2016-0018Ice phenomena on Lake Czarny Staw pod RysamiChoiński Adam0Department of Hydrology and Water Management, Adam Mickiewicz University, Krygowskiego 10, 61-680 Poznań, PolandDue to its inaccessibility (in winter), Lake Czarny Staw pod Rysami (Black Lake below Mount Rysy) has no series of continuous observations concerning ice phenomena. For the purpose of supplementing knowledge in this scope, ice corings were performed in the years 2010–2015. They permitted the determination of the variability of ice cover thickness on the lake’s surface. A high degree of similarity was determined in the distribution of ice cover thickness in the analysed winters (in contrast to the nearby Lake Morskie Oko). Moreover, a correlation was determined according to which the thicker the snow cover overlying the ice, the thinner the ice cover. It was determined that the mean thickness of the ice cover of Lake Czarny Staw pod Rysami is higher by approximately a dozen cm than that on Lake Morskie Oko located around 200 m lower.https://doi.org/10.1515/limre-2016-0018ice phenomenalake czarny staw pod rysamitatra mountains |
| spellingShingle | Choiński Adam Ice phenomena on Lake Czarny Staw pod Rysami Limnological Review ice phenomena lake czarny staw pod rysami tatra mountains |
| title | Ice phenomena on Lake Czarny Staw pod Rysami |
| title_full | Ice phenomena on Lake Czarny Staw pod Rysami |
| title_fullStr | Ice phenomena on Lake Czarny Staw pod Rysami |
| title_full_unstemmed | Ice phenomena on Lake Czarny Staw pod Rysami |
| title_short | Ice phenomena on Lake Czarny Staw pod Rysami |
| title_sort | ice phenomena on lake czarny staw pod rysami |
| topic | ice phenomena lake czarny staw pod rysami tatra mountains |
| url | https://doi.org/10.1515/limre-2016-0018 |
| work_keys_str_mv | AT choinskiadam icephenomenaonlakeczarnystawpodrysami |