Geoffrey Schladow

A global database of lake surface temperatures collected by in situ and satellite methods from 1985–2009

Global environmental change has influenced lake surface temperatures, a key driver of ecosystem structure and function. Recent studies have suggested significant warming of water temperatures in individual lakes across many different regions around the world. However, the spatial and temporal coherence associated with the magnitude of these trends remains unclear. Thus, a global data set of water temperature is required to understand and synthesize global, long-term trends in surface water temperatures of inland bodies of water. We assembled a database of summer lake surface temperatures for 291 lakes collected in situ and/or by satellites for the period 1985–2009. In addition, corresponding climatic drivers (air temperatures, solar radiation, and cloud cover) and geomorphometric characteristics (latitude, longitude, elevation, lake surface area, maximum depth, mean depth, and volume) that influence lake surface temperatures were compiled for each lake. This unique dataset offers an invaluable baseline perspective on global-scale lake thermal conditions as environmental change continues.

Tidal truncation and barotropic convergence in a channel network tidally driven from opposing entrances

Residual circulation patterns in a channel network that is tidally driven from entrances on opposite sides are controlled by the temporal phasing and spatial asymmetry of the two forcing tides. The Napa/Sonoma Marsh Complex in San Francisco Bay, CA, is such a system. A sill on the west entrance to the system prevents a complete tidal range at spring tides that results in tidal truncation of water levels. Tidal truncation does not occur on the east side but asymmetries develop due to friction and off-channel wetland storage. The east and west asymmetric tides meet in the middle to produce a barotropic convergence zone that controls the transport of water and sediment. During spring tides, tidally averaged water-surface elevations are higher on the truncated west side. This creates tidally averaged fluxes of water and sediment to the east. During neap tides, the water levels are not truncated and the propagation speed of the tides controls residual circulation, creating a tidally averaged flux in the opposite direction.

Effects of tidal current phase at the junction of two straits

Abstract Estuaries typically have a monotonic increase in salinity from freshwater at the head of the estuary to ocean water at the mouth, creating a consistent direction for the longitudinal baroclinic pressure gradient. However, Mare Island Strait in San Francisco Bay has a local salinity minimum created by the phasing of the currents at the junction of Mare Island and Carquinez Straits. The salinity minimum creates converging baroclinic pressure gradients in Mare Island Strait. Equipment was deployed at four stations in the straits for 6 months from September 1997 to March 1998 to measure tidal variability of velocity, conductivity, temperature, depth, and suspended sediment concentration. Analysis of the measured time series shows that on a tidal time scale in Mare Island Strait, the landward and seaward baroclinic pressure gradients in the local salinity minimum interact with the barotropic gradient, creating regions of enhanced shear in the water column during the flood and reduced shear during the ebb. On a tidally averaged time scale, baroclinic pressure gradients converge on the tidally averaged salinity minimum and drive a converging near-bed and diverging surface current circulation pattern, forming a “baroclinic convergence zone” in Mare Island Strait. Historically large sedimentation rates in this area are attributed to the convergence zone.

Erratum to: Climate variability and change in mountain environments: some implications for water resources and water quality in the Sierra Nevada (USA)

This article introduces this special journal issue on climate change impacts on Sierra Nevada water resources and provides a critical summary of major findings and questions that remain open, representing future research opportunities. Some of these questions are long standing, while others emerge from the new research reported in the eight research papers in this special issue. Six of the papers study Eastern Sierra watersheds, which have been under-represented in the recent literature. One of those papers presents hydrologic projections for Owens Valley, benefiting from multi-decadal streamflow records made available by the Los Angeles Department of Water and Power for hydrologic model calibration. Taken together, the eight research papers present an image of localized climatic and hydrologic specificity that allows few region-wide conclusions. A source of uncertainty across these studies concerns the inability of the (statistically downscaled) global climate model results that were used to adequately project future changes in key processes including (among others) the precipitation distribution with altitude. Greater availability of regional climate model results in the future will provide research opportunities to project altitudinal shifts in snowfall and rainfall, with important implications to snowmelt timing, streamflow temperatures, and the Eastern Sierra’s precipitation-shadow effect.

Modeling the transport of nutrients and sediment loads into Lake Tahoe under projected climatic changes

The outputs from two General Circulation Models (GCMs) with two emissions scenarios were downscaled and bias-corrected to develop regional climate change projections for the Tahoe Basin. For one model—the Geophysical Fluid Dynamics Laboratory or GFDL model—the daily model results were used to drive a distributed hydrologic model. The watershed model used an energy balance approach for computing evapotranspiration and snowpack dynamics so that the processes remain a function of the climate change projections. For this study, all other aspects of the model (i.e. land use distribution, routing configuration, and parameterization) were held constant to isolate impacts of climate change projections. The results indicate that (1) precipitation falling as rain rather than snow will increase, starting at the current mean snowline, and moving towards higher elevations over time; (2) annual accumulated snowpack will be reduced; (3) snowpack accumulation will start later; and (4) snowmelt will start earlier in the year. Certain changes were masked (or counter-balanced) when summarized as basin-wide averages; however, spatial evaluation added notable resolution. While rainfall runoff increased at higher elevations, a drop in total precipitation volume decreased runoff and fine sediment load from the lower elevation meadow areas and also decreased baseflow and nitrogen loads basin-wide. This finding also highlights the important role that the meadow areas could play as high-flow buffers under climatic change. Because the watershed model accounts for elevation change and variable meteorological patterns, it provided a robust platform for evaluating the impacts of projected climate change on hydrology and water quality.

Science-Based Decision Making in the Lake Tahoe Watershed

A close partnership between researchers, resources agencies, and community groups allows for the most effective ecological and economic approach to environmental protection and watershed management. One of the better documented examples of this type of cooperative effort comes from the Tahoe basin (CA-NV) where studies over the past four decades have shown that many factors including, land disturbance, habitat destruction, air pollution, soil erosion, roads, have interacted to degrade the Basins air quality, terrestrial landscape, and streams, as well as the lake itself. For effective lake management, we need to know (1) what are the specific sources of sediment and nutrients to the lake and what are their respective contributions, (2) how much of a reduction in loading is necessary to achieve the desired lake condition (lake response), and (3) how will this reduction be achieved? In this paper we present examples of ongoing research and monitoring which are proving extremely useful in watershed management. Topics include: changes in lake clarity and the importance of long-term data; response of lake phytoplankton to nutrients and a initial budget for nitrogen and phosphorus; paleolimnological reconstruction of baseline conditions and ecosystem response to anthropogenic disturbance; a clarity model to assess lake response to management; and a sediment transport model to evaluate nonpoint source loading. Only be providing a fully integrated watershed approach can we hope to develop effective restoration/mitigation efforts so essential to providing future generations with a quality environment in the Tahoe basin. Background The role of our nations universities in the evolving dialogue on watershed management is at a critical stage. Given the increased need to understand the (1) effects of pollution, (2) source(s), transport and fate of pollutants, and (3) continued public demand for clean air, land and water, these institutions are positioned to work closely with other stakeholders. A closer partnership between researchers, resources agencies, and community groups allows for a more effective ecological and more economic approach to environmental protection and watershed management. One of the better-documented examples of this type of cooperative effort comes from the Tahoe basin (CA-NV), where investigations by the Tahoe Research Group (TRG) at the University of California-Davis have provided clear evidence for the onset and progression of cultural eutrophication (Goldman 1988). Lake Tahoe is world-renowned for its clarity and water quality, however, continuous monitoring and research since the early 1960s has shown that algal growth is increasing at a rate greater than 5 percent per year. There has been a corresponding decline of clarity at an alarming rate of nearly one foot per year. This long-term trend in transparency is both statistically significant and is now perceivable to even the casual observer. Significant portions of the once pristine basin are urbanized. Studies by the TRG and others have shown that land disturbance, habitat destruction, air pollution, soil erosion, roads, etc. have all interacted to degrade air quality, terrestrial landscape, and streams, as well as the lake itself. We now know that once nutrients enter the lake they remain in the water, and can be recycled for decades (Jassby et al. 1995). As a consequence, the materials accumulate over time and contribute to Lake Tahoes progressive decline. The ability of Lake Tahoes large volume to dilute nutrient and sediment loading to levels where they have no significant affect on lake water quality has been lost.