Download presentation
Presentation is loading. Please wait.
Published byKennedy Denslow Modified over 10 years ago
1
When people care problems can be solved
2
LAKE TAHOE: A CASE STUDY FOR ADDRESSING THE DECLINE OF CLARITY IN A SUB-ALPINE LAKE JOHN REUTER and GEOFF SCHLADOW
3
Lake Tahoe UC Davis San Francisco Los Angeles
4
TAHOE ENVIRONMENTAL RESEARCH CENTER TERC conducts research, education and public outreach on lakes and their surrounding watersheds and airsheds. TERC provides objective scientific information for restoration and sustainable use of the Lake Tahoe Basin and inland waters in general. terc.ucdavis.edu
5
11000 sq ft labs, offices 1500 sq ft outreach 3000 sq ft class rooms
6
LAKE TAHOE BASIC FACTS 11 th deepest lake in the world Maximum Depth = 501 m Mean Depth = 330 m Lake Surface Area = 500 sq. km Watershed Area = 800 sq. km Shoreline length = 115 km Ultra-oligotrophic Monomictic 63 Inflowing streams 1 Outflowing stream Mean residence time ~ 600 yrs Altitude = 1895 m Latitude = 39 °N
7
Cause for Concern 30 m (100 ft target)
8
CONTRIBUTORS TO CLARITY DECLINE AT LAKE TAHOE
9
POLLUTANTS OF CONCERN Ultra-fine soil particles Nutrients and algal growth
10
Land disturbance - soil erosion
11
Wetlands Removal Before
12
After
13
Traffic Congestion Photo – Larry Prosor
14
Road Construction
15
Atmospheric Deposition
16
Angora Fire - 3100 acres burned - 253 homes lost
17
Stream Runoff
18
Urban Runoff
19
ORIGINALLY
20
NOW
21
Lake Tahoe Water Quality Management Approach l What is the problem and what causes it? l What are sources and relative contributions of nutrients and fine-sediments? l How much of a reduction is needed to achieve the desired conditions? l How will this reduction be achieved?
22
TMDL Overview Total Maximum Daily Load TMDL = science based water quality restoration plan
23
Nutrient & Fine Sediment Budget
24
Nitrogen
25
Phosphorus
26
Particle Number <20 µm
27
Lake Tahoe Clarity Model DLM Hydrodynamic/Thermodynamic Model Tributaries Climate, Precipitation Land Use Atmospheric Deposition Algal Growth Lake N, P, Si Inorganic Particles Loss Secchi Depth Light Scattering & Absorption Groundwater Tributaries Climate, Precipitation Land Use Atmospheric Deposition
28
WATER QUALITY INPUTS STREAMS [DO, BOD, CHLa, P (PP, THP, POP, RP), N (NO3, NH4, DON, PN, PON), # PART] G/WATER [P (THP, RP), N (NO3, NH4, DON), # PART] ATMOS [P ( THP, POP, RP ), N ( NO3, NH4, DON) ] PHYSICAL FORCING INPUTS MET [U, SW, LW, RH, T, PRECIP] STREAMS [Q, T] GROUNDWATER [Q] LAKE MODEL PHYSICS BIOLOGY
29
75% Reduction from Urban Runoff to Meet WQS of 30 m for Secchi Depth
30
Application to Grand Lake
31
Science should be part of decision-making
32
Importance of Data Knowledge Nice existing data base Future collection to answer specific questions to guide solutions (e.g. what is an appropriate target for water clarity?)
33
Solutions require: Shared responsibility Multi-year commitment Stakeholder participation
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.