skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Paleoclimatic significance of lake level fluctuations in the Lahontan Basin. [Pyramid Lake, Nevada]

Abstract

An energy flux balance model has been developed which treats evaporation as a function of air temperature, surface water temperature, precipitable water aloft, the amount, height, and type of sky cover, and the optical air mass. The model has been used to estimate the mean historical evaporation rate for Pyramid Lake, Nevada, using as input climatic data from the Reno area averaged over the period 1950 to 1975. Estimated and measured values of the mean annual evaporation rate were found to be in good agreement. The model was used to simulate changes in the level, the surface area and the volume of paleo Lake Lahontan. In particular, possible climatic states responsible for past high stands (1270 and 1330 m) were investigated. A conservative range of discharge values was used in the calculations. Results of the simulations indicate the fundamental importance of sky cover in the creation and destruction of large lake systems.

Authors:
Publication Date:
Research Org.:
California Univ., Berkeley (USA). Lawrence Berkeley Lab.
OSTI Identifier:
5073253
Report Number(s):
LBL-11265
DOE Contract Number:
W-7405-ENG-48
Resource Type:
Technical Report
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; LAKES; ENERGY BALANCE; NEVADA; AIR-WATER INTERACTIONS; CLIMATES; EVAPORATION; MATHEMATICAL MODELS; PALEONTOLOGY; SURFACE AREA; THEORETICAL DATA; VOLUME; DATA; INFORMATION; NORTH AMERICA; NUMERICAL DATA; PHASE TRANSFORMATIONS; SURFACE PROPERTIES; SURFACE WATERS; USA; WESTERN REGION; 520100* - Environment, Aquatic- Basic Studies- (-1989)

Citation Formats

Benson, L.V. Paleoclimatic significance of lake level fluctuations in the Lahontan Basin. [Pyramid Lake, Nevada]. United States: N. p., 1980. Web. doi:10.2172/5073253.
Benson, L.V. Paleoclimatic significance of lake level fluctuations in the Lahontan Basin. [Pyramid Lake, Nevada]. United States. doi:10.2172/5073253.
Benson, L.V. Fri . "Paleoclimatic significance of lake level fluctuations in the Lahontan Basin. [Pyramid Lake, Nevada]". United States. doi:10.2172/5073253. https://www.osti.gov/servlets/purl/5073253.
@article{osti_5073253,
title = {Paleoclimatic significance of lake level fluctuations in the Lahontan Basin. [Pyramid Lake, Nevada]},
author = {Benson, L.V.},
abstractNote = {An energy flux balance model has been developed which treats evaporation as a function of air temperature, surface water temperature, precipitable water aloft, the amount, height, and type of sky cover, and the optical air mass. The model has been used to estimate the mean historical evaporation rate for Pyramid Lake, Nevada, using as input climatic data from the Reno area averaged over the period 1950 to 1975. Estimated and measured values of the mean annual evaporation rate were found to be in good agreement. The model was used to simulate changes in the level, the surface area and the volume of paleo Lake Lahontan. In particular, possible climatic states responsible for past high stands (1270 and 1330 m) were investigated. A conservative range of discharge values was used in the calculations. Results of the simulations indicate the fundamental importance of sky cover in the creation and destruction of large lake systems.},
doi = {10.2172/5073253},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Fri Aug 01 00:00:00 EDT 1980},
month = {Fri Aug 01 00:00:00 EDT 1980}
}

Technical Report:

Save / Share:
  • Research conducted in the Chicago area over the past decade has resulted in detailed interpretation of changes. Stratigraphic studies, coupled with radiocarbon dating, indicate that conspicuous fluctuations of Lake Michigan have occurred during the past 2,000 years - a period previously recognized as one of relatively stable levels. Results of this study indicate a pattern of lake level changes not discernible in the 125-year historically recorded and measured changes; the historically recorded changes in lake level represent only part of a long-term, naturally fluctuating trend that in some cases may have exceeded the maxima and minima of the historically-recorded lakemore » levels.« less
  • The Sevier Lake Basin is a major land-locked drainage basin covering all or portions of 11 counties in southwest Utah and a small portion of one county in Nevada. The report provides information which the Federal Energy Regulatory Commission and its staff may use or build upon when considering matters related to hydroelectric project licensing, relicensing, or recommendation for Federal takeover. It enables the staff and the Commission to act expeditiously on matters pertaining to the development of the hydroelectric power potential of the Sevier Lake Basin within the limitations of other desirable water uses and environmental concerns. The economymore » of the Basin and existing water-resource and related land-resource developments are discussed, as well as the need for and a temporary survey of future development. (MCW)« less
  • The hydrology of Honey Lake Basin was studied using environmental isotope measurements of approximately 130 water samples collected during 1995 and 1996. The principal analytical methods included hydrogen, oxygen and carbon stable isotope ratio measurements, radiocarbon and tritium dating, and measurements of dissolved noble gas abundances.
  • This report presents the results of the Roach Lake Basin, Nevada, orientation study in the Kingman 1/sup 0/ x 2/sup 0/ quadrangle of the National Topographic Map Series (NTMS). Wet, dry, and playa sediment samples were collected throughout the 420 km/sup 2/ semi-arid, closed basin. Water samples were collected at the few available wells and springs. In addition to neutron activation analysis for uranium and 15 to 20 trace elements on all samples, field and laboratory measurements were made on water samples. Analytical data and field measurements are presented in tabular hardcopy and fiche format. Four full-size overlays for usemore » with the Kingman NTMS 1 : 250,000 quadrangle are included. Water sample site locations, water sample uranium concentration, sediment sample site locations, and sediment sample total uranium concentration are shown on the separate overlays. A general description of the area and the rock type distribution is presented. Some of the data in this report have been issued previously in ''Preliminary Report on the Roach Lake Pilot Study,'' GJBX-44(76), August 1976.« less
  • The Lawrence Livermore Laboratory (LLL) is conducting a hydrogeochemical and stream-sediment survey in the seven western states as part of ERDA's National Uranium Resources Evaluation (NURE) Program. The objective of this survey is to develop a geochemical data base for use by the private sector to locate regions of anomalous uranium content. Prior to wide area coverage, several pilot studies are being undertaken to develop and evaluate sampling and analytical techniques. The second through fifth of these studies were conducted in four playa basins in Neveda, selected to represent different regional geology and uranium occurrence. This study in the Roachmore » Lake Basin characterizes carbonate surface lithology containing known uranium occurrences. Roach Lake is surrounded by several areas of carbonate terrain, the most important of which is the Spring Mountain Range to the north and west. These mountains contain the Goodsprings Mining district, noted for lead, zinc, and copper mines. Many of these mines contain uranium minerals within the oxidized sulfide zone. Mineralization is mainly confined within the Mississippian limestone. The basin drains an area of 250 square miles and is bounded on the east by the McCullough Range. The study area is typical of the eastern portion of the Basin and Range province and should be relevant to southeastern Idaho, the western half of Utah, central and eastern Nevada, small portions of northwest Arizona, and a portion of southeast California. This report contains only the analytical data and sample locations.« less