3 edition of Climatological observations, water levels, and water temperatures, Iliamna Lake, Alaska, 1971 found in the catalog.
Climatological observations, water levels, and water temperatures, Iliamna Lake, Alaska, 1971
Loh Lee Low
by Fisheries Research Institute, College of Fisheries, University of Washington in Seattle
Written in English
|Statement||by Loh Lee Low.|
|Series||Fisheries Research Institute circular -- no. 72-5, Circular (University of Washington. Fisheries Research Institute) -- no. 72-5.|
|Contributions||University of Washington. Fisheries Research Institute., United States. National Marine Fisheries Service.|
|The Physical Object|
|Pagination||33 p. :|
|Number of Pages||33|
Alaska Salmon Supply -T -i U) § n ^—» £ E ° T3 S CD ' ow W g 50 n O C\l ^~ CD CO O CM -^- CD CO O CM * CD CO ^0^0^0^ O^ O^ O} O} O} O} O} O} O} O} ^D ^D ^D ^D ^D • Total Alaska coho & chinook • Total Alaska chum • Total Alaska pink • Other Alaska sockeye • Bristol Bay. climate change. In lake-rich regions, the loss of ice cover also plays a key role in landscape and climatic processes. Thus, there is a need to understand lake ice phenology at multiple scales. In this study, we observed ice-out timing on 55 large lakes in 11 lake districts across Alaska from to using satellite imagery. Sensor networks inCited by:
Allowable pairs of precipitation and evaporation can then be estimated for any past lake level. Particularly in cases where precipitation is the primary control of water depth, it is possible to model lake level responses to past changes in precipitation (e.g., Cited by: The map below shows the near real-time water temperatures in degrees Fahrenheit (°F). Use the near real-time water temperature data with discretion, because they may contain errors. Click on a station marker for the near real-time and monthly mean temperature of the station. Water Temperature Map of the Alaska Coast (Table-based Web page).
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Climatological observations, water level and water temperatures, Iliamna Lake, Alaska, (University of Washington. Fisheries Research Institute.
Circular) [William H Lenarz] on *FREE* shipping on qualifying offers. Climatological observations, water level, and water temperatures, Iliamna Lake, Alaska, (Fisheries Research Institute circular) [GunnerÃ, d, Tor B] on *FREE* shipping on qualifying offers.
Climatological observations, water level, and water temperatures, Iliamna Lake, Alaska, (Fisheries Research Institute circular). Buy Climatological observations, water level, and water temperatures, Iliamna Lake, Alaska, (Fisheries Research Institute circular) by Gunnerød, Tor B (ISBN:) from Amazon's Book Store.
Everyday low prices and free delivery on eligible : Tor B Gunnerød. Climate warming increases vertical and seasonal water temperature differences, and inter-annual variability in a mountain lake Article (PDF Available) in Climatic Change. Buy Climatological observations, water level and water temperatures, Iliamna Lake, Alaska, (University of Washington.
Fisheries Research Institute. Circular) by William H Lenarz (ISBN:) from Amazon's Book Store. Climatological observations low prices and free delivery on eligible : William H Lenarz.
The warming climate has caused increases in 1971 book temperature, decreases in the extent and duration of ice cover, and altered water levels, which. A rapid~18 m rise in water levels at Birch Lake, south of Fairbanks at~15 ka (Fig.
9; Abbott et al., ) and rising and higher lake levels at nearby Harding Lake by~14 ka (Finkenbinder et. At Birch Lake, interior Alaska, trends in aquatic taxa and sediment characteristics for the last ca.
12, ^14C yrs recorded in a single, deep-water core reflect the same water-level changes as. Historical observations from Harding Lake demonstrate lake level fluctuations on the order of several meters since the 's (LaPerriere, ), with periodic exposure of the shallow shelf along the northern shore.
Given the substantial water depth of the depocenter at Harding Lake (>42 m), this deep core site appears relatively insensitive to Cited by: These are the stations in Alaska with the best historical climate information.
Click on the map or on the list below the map for information on the local topography, station history, and mean annual temperature history. Temperature and precipitation normals as a function of time of year are available for many of these sites at the CDC Climate site.
Iceberg Lake 4 is an ice-dammed proglacial lake in the eastern Chugach Mountains of Alaska ().The m-deep, km 2 lake sits amidst high topography of the eastern Chugach mountains on the Chugach terrane, midway between the Border Ranges Fault to the north and the Contact Fault to the south (Plafker et al., ).Large contiguous icefields characterize the region, Cited by: The effects of water color on lake stratification, mean epilimnetic irradiance, and lake temperature dynamics were examined in small, north-temperate lakes that differed widely in water color ( Temperature and precipitation of Alaska: 50 year trend analysis J.
Stafford, G. Wendler, and J. Curtis With 8 Figures Received Aug Revised Ma Summary Temperature and precipitation records from to were examined for 25 stations throughout the State of Alaska. Mean, maxima, and minima temperatures, diurnal. A 14, yr high-resolution pollen and lake-level record from Windmill Lake in central Alaska provides new evidence for the Late Pleistocene and Holocene paleoenvironments of this region.
At 14, 14 C yr BP, sparse herb tundra and low lake-levels indicate a cold, arid by: Tor B. Gunnerød, 3 books Loh Lee Low, 2 books Anderson, John W., 1 book Orra Edwin Kerns, 1 book Linda K.
Brannian, 1 book Gary W. Miller, 1 book. The Alaska Climate Research Center is a research and service organization at the Geophysical Institute, University of Alaska Fairbanks. Our group conducts research focusing on Alaska and polar regions climatology and we archive climatological data for Alaska.
NWIS Water Temperature in Celsius (Where Available) for the Week in Lake Iliamna - HUC USGS Drought Watch - U.S Map of Drought and Low Flow Conditions USGS WaterWatch - Real-time Streamflow Map for the Alaska Region- HUC in the flow regimeor creation of a reservoir can alter water temperatures, dissolved gases, nutrients, turbidity/light, and the bioavailability of contaminants within a river.
- Such changes can affect all trophic levels. Water temperatures limit and/or determine the distribution and abundance of many riverine Size: 6MB.
A new "blob", or large area of warm water observed in the Gulf of Alaska, named the Northeast Pacific Marine Heatwave offormed in May and reached its maximum size in August. It has since decreased in size and intensity, but is still one of the most significant events seen in the past 40 years.
The September minimum sea ice extent. winter temperatures and ice conditions mean daily air temperature for january in °c 0 • -5 i i ' maximum ice cover in tenths 10 [solid ice) 7- 9 1 • 6 0 (open water) frost free period and air masses mean annual frost free period in days i.
For Lake Tahoe events prior to October (i.e., 9 events) and all Pyramid Lake events (i.e., 36), biweekly climatological water temperatures for each lake were used.
A comparison of mean water temperatures for Lake Tahoe LE events after October (i.e., 17 events) with biweekly climatological water temperatures found the observed event Cited by: 2.Sponsor a Book.
Fisheries Research Bathymetric measurements of Iliamna Lake and Lake Clark, Alaska Anderson, John W. Read. Distances from sea and elevation of important sockeye salmon spawning Patrick H. Poe Climatological observations, water levels, and water temperatures, Ili.Larger body size and earlier run timing increase alewife reproductive success in a whole lake experiment,Canadian Journal of Fisheries and Aquatic Sciences (76) - 7 Phenology of hatching, emergence, and end-of-season body size in young-of-year Coho Salmon in thermally contrasting streams draining the Copper River Delta, Alaska,