Water stage dynamics in Lake Wielki Staw in the Valley of Five Polish Lakes

Abstract

The paper presents an analysis of water stages in Lake Wielki Staw based on observations by the Institute of Meteorology and Water Management conducted in the years 1968-1979. Water level (low and high) variability was determined in the annual cycle, together with the variability of annual stages in the analysed 12-year period, and their amplitudes. Moreover, water stage variability trends were identified. Due to the vicinity of Lake Morskie Oko, comparisons of water stages in both lakes were performed for the purpose of determining the degree to which water supply (water stages) is affected by local and climatic factors.

Water stage dynamics in Lake Wielki Staw in the Valley of Five Polish Lakes

Limnol. Rev. (2016) 16, 1: 27-31

DOI 10.2478/limre-2016-0003

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Water stage dynamics in Lake Wielki Staw in the Valley of Five Polish Lakes

Adam Choiski

Department of Hydrology and Water Management, Adam Mickiewicz University, Dzigielowa 27, 61-680 Pozna, Poland, e-mail: [email protected]

Abstract: The paper presents an analysis of water stages in Lake Wielki Staw based on observations by the Institute of Meteorology and Water Management conducted in the years 1968-1979. Water level (low and high) variability was determined in the annual cycle, together with the variability of annual stages in the analysed 12-year period, and their amplitudes. Moreover, water stage variability trends were identied. Due to the vicinity of Lake Morskie Oko, comparisons of water stages in both lakes were performed for the purpose of determining the degree to which water supply (water stages) is aected by local and climatic factors.

Key words: water stages, lake hydrology, Tatra Mountains

Introduction

Research on high mountain lakes (Lake Wielki Staw in the Valley of Five Polish Lakes is categorised as such in Polish conditions) is exceptionally difficult due to their inaccessibility. This particularly concerns the winter period, when access is practically impossible because of the thick layer of snow and threat of avalanches. The only possibility to obtain continuous observation data is the establishment of a shelter functioning all year round on the shore of such a lake, permitting frequent and safe access of the observer to the shore. One of a few such examples in the Tatra Mountains is the shelter in the Valley of Five Polish Lakes (Schronisko Piciostawiaskie). At an altitude of 1671 m a.s.l, this shelter is the highest in Poland . It is built on the shore of Lake Przedni Staw, but only 400 m from Lake Wielki Staw. This position permitted year-round measurements of the largest of the ve lakes, i.e. Lake Wielki Staw. In addition to the analysed lake, permanent observations in the Polish Tatra Mountains have been or are conducted only in Lake Zielony Staw on Hala Gsienicowa (Gsienicowa Glade) and Lake Morskie Oko.

Study object and methods

Due to its location and the morphometric parameters of its basin, Lake Wielki Staw in the Valley of Five Polish Lakes stands out among more than 7 thousand Polish lakes. It is located at an altitude of 1664.6 m a.s.l. (water surface level 1662.85 m above Kr., mean state from multiannual 180 cm), i.e. 268.8 m above the level of Morskie Oko. It is the deepest lake in the Tatra Mountains 80.3 m (Choiski 2000), and third largest lake in Poland. In terms of mean depth, i.e. 37.7 m, it is second aer Lake Hacza (38.7 m), and in terms of mean bottom inclination, it occupies the fourth position (Choiski 2007). In terms of surface area, Wielki Staw is second in the Polish Tatra Mountains aer Morskie Oko. Its basin accumulates the highest volumes of water, i.e. approximately 13 hm3. The catchment area is small, occupying 5.5 km2. The lake is surrounded by high peaks (e.g. Kozi Wierch 2291 m a.s.l. located only 1.1 km in straight line from Lake Wielki Staw) rising 500-600 m above the water surface. The scarcity of vegetation in the conditions of such high slopes permits very fast surface runos, i.e. a rapid response of the lake to intensive rainfall. The

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lake is fed by several small streams from the southwest. The Roztoka Stream ows out of the lake on its northern edge.

On 1 November 1967, the Institute of Meteorology and Water Management initiated observations of water stages in ve-day intervals. They lasted until the end of October 1979. Therefore, they cover (continuously) 12 hydrological years. The results of the observations are published in hydrological yearbooks of surface waters (IMGW 1968-1979). Data for the years 1968-1970 are presented in the form of monthly means, and for the remaining years as measurements performed every ve days. Moreover, observations of ice phenomena were conducted. In spite of the short observation term, the analysis of the obtained results seems to be strongly justied. It is the highest located hydrological object in Poland subject to continuous observation.

The objective of the paper is: to determine water level uctuations in the annual and multiannual course, to determine the existence of tendencies of changes and its character, and to compare the dynamics of water stages in Lakes Wielki Staw and Morskie Oko. This may help determine whether the response of the lakes to alimentation is only determined by the climatic factor, or whether local conditions considerably aect the size and rate of alimentation. It should be mentioned that in terms of surface area, both lakes dier by only a few percent. The same concerns the area of their catchments. Therefore, the main factor determining evident dierences between them is the height of the water surface above sea level, but potentially also various conditions of the catchment such as ground absorbency, slope inclinations, contribution of areas covered with vegetation, etc.

Results and discussion

Water stages in Lake Wielki Staw in the multi-annual period show very high dynamics. The highest observed daily water stage in the lake in the winter half-year amounted to 205 cm (30 April 1968), and in the summer half-year to 253 cm (29 July 1968). The lowest stages amounted to: 165 cm (1, 5 November 1969, 25 January 1973) and 164 cm (20 October 1969), respectively. The extreme amplitude over such a short observation term, i.e. 12 years, amounted to as much as 89 cm. On the country-wide scale , this is an exceptional value, because only approximately a dozen lakes show a greater scale of water level uctuations. Con-

sidering this near half a metre water level uctuation and the lakes surface area, it can be presumed that the dierence in the volume of the lake at maximum and minimum stages amounts to approximately 305 dam3.

Due to the exceptional mean depth, the water volume within the range of the amplitude is equivalent to only approximately 2.3% of total water resources. The mean water stage for the summer half-year (186 cm) in the analysed multiannual is higher than the mean stage for the winter half-year (173 cm) by 13 cm.

The course of maximum, mean, and minimum stages, as well as amplitudes in the years 1968-1979 are shown in gure 1. In the case of Lake Wielki Staw, the maximum level is statistically signicant at a decreasing trend (p < 0.05, r2 = 0.45). The situation is similar in the case of amplitudes (p < 0.05, r2 = 0.57). In the case of low stages, a statistically signicant increasing trend occurs (p < 0.05, r2 = 0.53). In the case of mean stages, the increasing trend is not statistically signi-cant (p > 0.05, r2 = 0.23). In the case of Lake Morskie Oko, decreasing trends occur for all parameters, statistically signicant for the maximum (p < 0.05, r2

= 0.40) and mean value (p < 0.05, r2 = 0.58). In the case of the minimum value and amplitudes, the trends were not statistically signicant (respectively: p > 0.05, r2 = 0.05; p > 0.05, r2 = 0.28).

The variability of water stages (every ve days for hydrological years 1971-1979) against the background of daily amounts of atmospheric precipitation is compared in gure 2. It marks the duration of the persistence of ice phenomena which are twofold, i.e. in the above case they include periods of occurrence of compact ice cover and oating ice. The course of water stages in Lake Wielki Staw over the year is generally twofold. The rst period corresponds to the occurrence of ice phenomena. The lake is isolated in summer from the direct impact of external conditions (e.g. precipitation, surface runos, wind-induced water level increases). This results in a relative stability of water stages. The mean duration of ice phenomena (for the years 1971-1979) amounted to 200 days, including that of ice cover of 167 days. The longest occurrence of ice phenomena in the period amounted to 227 days (1975), and the shortest to 170 days (1971). The values for ice cover are 205 days (1975) and 141 days (1977), respectively. Water level uctuations under the ice are low, and for the rst three months with ice phenomena they are within a range of approximately 10 cm. From the turn of February and March a permanent increase in the water level usually occurs, with a culmination in

Water stage dynamics in Lake Wielki Staw in the Valley of Five Polish Lakes

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Fig. 1. Course of maximum, average, and minimum stages, and amplitudes for Lakes Wielki Staw (A) and Morskie Oko (B)

May or June. This corresponds to the end of the occurrence of ice phenomena, and to intensive snowmelts. An exception to the rule was 1973, when the water level under ice was stable until almost the end of April. The increase in the water level under the ice from the turn of February and March is interesting. It signies the beginning of melting of snow, permafrost, and the bottom of the ice cover, resulting in an increase in the lakes alimentation. In certain years the culmination of the annual water level results from snowmelt, e.g. the years: 1975, 1976, 1977, and 1979. The dierence in the water levels between minimum stages (usually occur-ring in February) and those resulting from snowmelt

vary from 30 to 40 cm. Summer precipitation culminations occurred somewhat more frequently than snowmelt culminations. This concerns the years: 1971, 1972, 1973, 1974, and 1978.

Aer the snowmelt period the water level decreases by approximately 20-30 cm until the moment of intensive rainfall, which usually causes a rapid increase in the water level in the lake. The period between the spring snowmelt culmination and summer rainfall culmination is largely varied. In 1974 and 1979, it was only one month, in 1971 and 1977 two months, in 1978 three months, and in 1976 four months. In certain years evident summer culmina-

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tions occur twice, e.g. in 1973 and 1974. In addition to their violent character, summer maximums are also distinguished by short duration (usually several to approximately a dozen days) and considerable height, i.e. up to more than 60 cm (1973). The responses of the lakes water level to the amount and intensity of rainfall are very diverse. In some cases: in spite of substantial precipitation totals, the response of the water level is inconsiderable (e.g. 1976, 1979),

the response of an increase in the lakes water level to precipitation is immediate and considerable (e.g. July 1971, June and August 1973, August 1978),

an inconsiderable decrease in the water level oc-curs in spite of substantial precipitation (e.g. August 1971, June 1978),

in spite of substantial precipitation, the response of the water level is inconsiderable or non-existent (September 1972, September 1973, September 1974, July 1975),

rainfall occurs in the period of snowmelt in the nal phase of ice phenomena (e.g. May 1972, June 1975).

Fig. 2. Water stages in Lake Wielki Staw against the background of daily precipitation totals and duration of ice phenomena. Explanations: 1 daily precipitation totals, 2 water stages, 3 compact ice cover, 4 oating ice (according to data of the Institute of Meteorol-

1 daily precipitation totals, 2 water stages, 3 compact ice cover, 4 oating ice (according to data of the Institute of Meteorology and Water Management; precipitation for station Morskie Oko)

The diversity of the aforementioned situations results from a number of factors, such as the varied state of retention of weathered rock covers at a given moment, varied temperatures of rocks on the surface determining the volume of evaporation, and varied water levels in the lake at the moment of the occurrence of precipitation.

Conclusion

Lake Wielki Staw in the Valley of Five Polish Lakes in the years 1968-1979 was the highest located hydrological object in Poland subject to continuous observations by the Institute of Meteorology and Water Management. The amplitude of extreme stages is very high. Over 12 years of observations, it increased by as much as 89 cm. For Lake Morskie Oko, the analogical value amounted to 111 cm (although for a longer period, i.e. 47 years) (Pociask-Karteczka et al. 2014). Water stages in Lake Wielki Staw in the annual course are evidently twofold, i.e. the rst period corresponds with the occurrence of ice phenomena with a mean yearly duration amounting to 200 days.

Water stage dynamics in Lake Wielki Staw in the Valley of Five Polish Lakes

For the rst three months of their duration, water level uctuations are stable, i.e. they equal up to 10 cm. From the turn of February and March, the water level continuously increases, with a culmination in the nal phase of the occurrence of ice phenomena, i.e. during intensive snowmelt. The lake released from ice responds to rain alimentation in very diverse ways. Annual culminations of water stages are reached both as snowmelt and rainfall culminations in summer, whereas the former amount to 30-40 cm, and the latter to even more than 60 cm. Summer culminations of water stages can be inconsiderable, but can occur several times. In the case of Lake Morskie Oko, the course of maximum, mean, and minimum stages, as well as amplitudes shows a decreasing trend, and for Lake Wielki Staw the course of maximum stages and amplitudes shows a decreasing trend, and for low and mean stages an increasing trend.

Acknowledgements

I would like to thank Ms. M.Sc. Alicja Baczyska and Mr. Prof. Dariusz Wrzesiski for help in the preparation of the gures.

References

Choiski A., 2000, Najgbsze jeziora Tatr polskich w wietle najnowszych pomiarw gbokociowych (The deepest lakes of the Polish Tatra Mountains in light of recent bathymetric measurements), Czas. Geogr. 71(1): 99-103 (in Polish, English summary).

Choiski A., 2007, Limnologia zyczna Polski (Physical

Limnology of Poland), Wyd. Nauk. UAM, Pozna, 540 pp (in Polish).

[IMGW] Instytut meteworologii i Gospodarki Wodnej (Institute of Meteorology and Water Management), 1968-1979, Rocznik hydrologiczny wd powierzchniowych. Dorzecze Wisy i rzek Przymorza na wschd od Wisy (Hydrological yearbook of surface waters. The Wistula basin and the rivers of the coast region east of the Vistula River), WKi, Warszawa (in Polish).

Pociask-Karteczka J., Choiski A., Nieckarz Z., 2014, Dynamika stanw wody (The dynamics of water stages), [in:] Choiski A., Pociask-Karteczka J. (eds) Morskie Oko przyroda i czowiek (Morskie Oko: nature and a man), Wyd. TPN, Zakopane: 38-49 (in Polish).

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