SENECA LAKE
A view form the western shore
Photo: C. Rossano
A. LOCATION
New York, USA. 42:2 N, 76:6 W; 135.6 m above sea level.
B. DESCRIPTION
Seneca Lake is one of a group of long and narrow lakes
located in western New York State known as the Finger Lakes. The basins
of these north-south oriented lakes were formed by the advance of ice masses
during the Ice Ages, and further sculpted by glacial meltwater during the
interglacial and postglacial periods. Seneca Lake is 56.6 km long, has
a mean width of 3.10 km, and a mean depth of 88.6 m. Seneca Lake is by
far the deepest of the Finger Lakes (198.4 m); with the lake floor extending
more than 60 meters below sea level. As a result, Seneca Lake's volume
is by far the greatest (15.539 km3); and retention time longest (18.1 yr)
of the Finger Lakes.
Although the Finger Lakes region is now well-known
for its many vineyards and orchards, it had been densely forested up until
the early 1800's when large areas were cleared for agriculture by white
settlers. The forests are now in the process of expanding as marginal farmland
is abandoned and gradually invaded by trees.
Of Seneca Lake's 1,180 km2 drainage basin, approximately
40% is forested, 40% is actively farmed, and 3% is residential. Approximately
70,000 people were residing in the drainage basin in 1970.
The climate of the Finger Lakes region is characterized
by cold, snowy winters and warm, dry summers; and occasionally the lake
freezes over in January or February. However, because the water in the
lake acts as a heat-regulator, and because the land surrounding the lake
is steeply sloped, Seneca Lake actually has a considerable effect on the
local climate. These factors interact to moderate the seasonal temperature
extremes and variability within the lake valley. Consequently, the slopes
surrounding the lake are ideally suited for growing fruit (1).
C. PHYSICAL DIMENSIONS (1)
Surface area [km2] |
175 |
Volume [km3] |
15.5 |
Maximum depth [m] |
198.4 |
Mean depth [m] |
88.6 |
Residence time [yr] |
18.1 |
Catchment area [km2] |
1,831 |
D. PHYSIOGRAPHIC FEATURES
D1 GEOGRAPHICAL (1) Bathymetric map: Fig. NAM-16-0l. Names of main
island: None. Number of outflowing rivers and channels (name): 1.
D2 CLIMATIC Climatic data at Geneva, 1933-1962 (2)
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Mean temp. [deg C] |
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Jan
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Feb |
Mar |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
Ann. |
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-3.3 |
-3.3 |
1.1 |
7.8 |
14.4 |
19.2 |
22.2 |
21.1 |
17.2 |
11.1 |
5.0 |
-1.7 |
9.2 |
Number of hours of bright sunshine (Binghamton): 612 hr yr-1 (3). Snowfall
(Binghamton): 132 mm (3).
Fig. NAM-16-01
Bathymetric map (1).
Solar radiation: Fig. NAM-16-02.
Fig. NAM-16-02
Pooled quadratic curve for solar radiation near Geneva, New York (2).
Water temperature [deg C](1) 1973
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Depth[m] |
Jan |
Feb |
May |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
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S*1 |
- |
- |
- |
5.6 |
- |
- |
23.5 |
23.5 |
- |
- |
- |
- |
B*2 |
- |
- |
- |
4.0 |
- |
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4.0 |
5.5 |
- |
- |
- |
- |
*1 Surface. *2 Near bottom. Mixing type: Monomictic (1).
E. LAKE WATER QUALITY (1)
E1 TRANSPARENCY [m] 1973: 3.6*. * Summer Secchi disc transparency.
E6 CHLOROPHYLL CONCENTRATION [micro g l-1]: Fig. NAM-16-03.
Fig. NAM-16-03
Chlorophyll a and phaeopigments concentrations during the 1973 synoptic
survey.
F. BIOLOGICAL FEATURES (1)
F1 FLORA Submerged macrophytes Myriophyllum spicatum, Heteranthera
dubia, Potamogeton crispus, P. perfoliatus, Chara sp. Phytoplankton Ankistrodesmus
falcatus, Golenkinia radiata, Oocystis lacustris, Scenedesmus armartus,
Ceratium hirundinella, Glenodinium borgei, Cryptomonas erosa, Cladomonas
fruticulosa, Mallomonas akrokomas.
F2 FAUNA Zooplankton Diaptomus minutus, D. oregonenis, Cyclops
bicuspidatus, Bosmina longirostris, Ceriodaphnia quadrangula, Mysis relicta,
Asplanchna priodonta, Synchaeta stylata. Benthos Pontoporeia hoyi, Chiromomus,
Tanypus, Palpomyia, Protenthes, Sphaerium. Fish Alosa pseudoharengus, Salmo
gairdneri, Salvelinus namaycush, Cyprinus carpio, Catostomus commersoni,
Ictalurus nebulosus, Esox lucius, Hypentelium nigricans, Ambloplites rupestris.
F4 BIOMASS: Fig. NAM-16-04.
Fig. NAM-16-04
Phytoplankton cell numbers during the 1973 synoptic survey.
G. SOCIO-ECONOMIC CONDITIONS (1)
G1 LAND USE IN THE CATCHMENT AREA
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Area [km2] |
[%] |
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Natural landscape |
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Forest |
476.5 |
40 |
Agricultural land |
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Active agriculture |
501.5 |
43 |
Inactive agriculture |
165.5 |
14 |
Residential area |
37.1 |
3 |
Total |
1,180.6 |
100 |
Main types of woody vegetation (main species) Northern hardwoods (Fagus
grandifolia, Acer saccharum), Elm-red maple-northern hardwoods (Ulmus americana,
Acer rubrum), Oaknorthern hardwoods, Pine-oak-northern hardwoods.
G3 POPULATION IN THE CATCHMENT AREA
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Total no. Increase |
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Population density |
1930 |
1970 |
[%] |
[km-2] |
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44,561 |
69,559 |
56 |
58.9 |
I. DETERIORATION OF LAKE ENVIRONMENTS AND HAZARDS
I3 EUTROPHICATION Nitrogen and phosphorus loadings to the lake [g
m-2 yr-1](4) T-P: 0.64.
Fig. NAM-16-05
(1) Nitrogen loadings (LSN) to eight of the Finger Lakes.
J. WASTEWATER TREATMENTS (1)
J3 SANITARY FACILITIES AND SEWERAGE Discharge of the City of Geneva's
primary sewage treatment plant ca. 7,600 day-1.
N. SOURCES OF DATA
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Schaffner, W. R. & Oglesby, R. T. (1978) Limnology of eight Finger
Lakes: Hemlock, Canadice, Honeoye, Keuka, Seneca, Owasco, Skaneateles,
and Otisco. "Lakes of New York State 1, Ecology of the Finger Lakes" (ed.
Bloomfield, J. A.), pp. 313-470. Academic Press, New York, San Francisco,
London.
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Stephen, W. E. & Larry, P. K. (1978) The Limnology of Canandaigua Lake.
Ibid. pp. 225-311.
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Court, A (1974) The climate of the conterminous United States. "World Surveys
of Climatology, Volume 11, Climates of North America" (ed. Bryson, R. A.
& Hare, F. K.), p. 312. Elsevier Scientific Publishing Company, Amsterdam-London-New
York.
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Oglesby, R. T. & Schaffner, W. R. (1975) The response of lakes to phosphorus.
"Nitrogen and Phosphorus Food Production, Waste and the Environment" (ed.
Porter, K. S.), Chapter 2, pp. 25-57. Ann Arbor Sci. Publ., Ann Arbor,
Michigan.