| Title | Description | Research Sites | Related Links |
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| Douglas Lake Water Profiles |
Water temperature and dissolved oxygen profiles for various parts of Douglas Lake. These profiles span a number of investigators, time periods and locations within Douglas Lake so pay attention to the Dataset details. |
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| Phenology shifts in northern forest ecosystems |
Large-scale phenological shifts, or timing of key life events, have been observed across many ecosystems and are consistent with changes expected with climate change. With annual temperature increases of roughly 0.2 degrees C, advancement in the timing of budburst and flowering have been widely observed. Earlier budburst and therefore longer growing seasons may have significant implications for carbon storage. Previous research has shown that increases of only one day in growing season have significantly increased forest net ecosystem productivity (NEP). However, the relationship between earlier budburst and NEP is not well established. Kellen’s research will examine the connection between phenological events at the species levels and phenological timing at the stand scale. In contrast with the more evident relationship among increased temperature, earlier onset of budburst, and increased NEP, the connections between phenology and local, boundary-layer meteorology are much less understood. Leaf-out has been correlated with a wide variety of meteorological components including temperature, vapor pressure, and relative humidity. Kellen’s research will use precise phenological and meteorological observations to develop climate-biosphere models and determine the effects of phenological shifts on the climate-biosphere linkage so these findings can be incorporated into climate models. Changes in timing of autumnal senescence have also been widely observed, although changes are more variable between ecosystems and more poorly understood than budburst events. Delayed leaf abscission may cause incomplete resorbtion of nutrients to storage organs as well as less N. 1. Have shifts in the timing of spring phenology occurred at Wauseon, OH in comparison to legacy data sets from the 1880's-1913? 2. How will shifts in both spring and autumn phenology impact carbon storage dynamics in northern forest ecosystems with the shift from aspen and birch dominated canopies to more heterogeneous oak and maple forests? 3. How will shifts in timing of leaf fall impact nutrient resorption dynamics? 4. What are key meteorological drivers of phenological events? |
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| Modelling forest growth, succession, and biogeochemistry to study the effects of disturbances on forest carbon cycling |
Due to heavy logging and intense fires at the beginning of the twentieth century, the forests at UMBS are characterized by an early successional state dominated by short-lived tree species such as aspens and birches. As these species approach the end of their life span, they are expected to die off and be replaced by longer-lived, more shade-tolerant species such as white pine and red oak. These successional changes happen over a long time scale that is difficult to resolve with field observations, and may have important impacts on carbon, nutrient, and water budgets in the forests at UMBS. I am using a combination of measurements and computer modeling to characterize the effects of succession on CO2 and volatile organic compound (VOC) fluxes to the atmosphere. I am using the LANDIS-II computer model to develop predictions of future carbon budgets at UMBS. This model simulates tree growth, establishment, mortality, and succession. The model will be parameterized using CO2 flux measurements from the FASET and Ameriflux towers, as well as aboveground biomass measurements from a number of permanent plots. The historical data from these plots will help to constrain model predictions of long-term biomass accumulation. VOC flux predictions will be constrained using measurements from a relaxed eddy accumulation (REA) system. Measurements were conducted at both the FASET and PROPHET towers in order to measure the differences in VOC emissions between forest successional stages. |
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| Plant responses to herbivory |
Plants respond to herbivory by evolving and inducing defenses against herbivores. Though plant defenses have been studied extensively, indirect defenses have neither been incorporated into theories of plant defense, nor investigated alongside direct defenses. Volatile organic chemicals (VOCs) are gases which can be emitted by vegetation. They play an important role in biosphere-atmosphere dynamics as well as in community interactions. VOCs have been shown to contribute to indirect plant defense against herbivores by attracting predators and parasitoids (higher trophic levels) to their herbivore hosts; however, the adaptive role of these plant signals in defense has not yet been shown convincingly. Genetic and environmental variables, as well as community context, can influence plant VOC emission. For my dissertation work, I intend to implement field and greenhouse experiments in order to gauge the relative roles of genetic variation, environmental factors, atmospheric processes, community context, geographic variation, and herbivory in influencing plant VOC emission; integrate plant VOC emission into current models of plant defense theory; and determine whether VOC emission evolved as an adaptive response to herbivore damage. |
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| Inclusion of vegetation in climate models |
The inclusion of vegetation in climate models is key to understanding and simulating future climate change. Vegetation processes are often parametrized through leaf temperature yet very few measurements are available for model evaluation. The proposed work will conduct leaf temperature measurements in summer 2010 at the UM Biological Station, and results will be used to develop a new, experimental research avenue for the PI. Funds will support one graduate student and provide field equipment and travel to UMBS. |
UMBS AmeriFlux Tower | |
| RANN: Research Applied to National Needs |
In the early 1970s the University of Michigan Biological Station initiated a series of research projects concerning the quality of the lakes in Northern Michigan under the support of the National Science Foundation through the Research Applied to National Needs (RANN) program. Dr. John Gannon joined the Biological Station's staff in 1972 and directed this program for six years. This research had significant impacts on water quality management of lakes throughout Northern Michigan. The Biological Station continued to receive grants for water quality research for several years after the RANN program had terminated. |
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Map of lakes surveyed from 1972 - 1975 |
| Ozone reactivity rates with respect to biogenic volatile organic compounds (VOC) |
A three week experiment associated with the CABINEX project based around the PROPHET tower. Project goal is to examine ozone reactivity rates with respect to biogenic volatile organic compounds (VOC). Comparison of these measured reactivity rates with lab studies may suggest that there are unaccounted reactions taking place that are currently not understood. Using branch enclosure techniques to isolate biogenic VOC emissions, ozone will be introduced to reactivity chambers and allowed to react. Using differential ozone monitors, ozone reactivity rates with respect to VOC reactions may be determined. Additionally, VOC samples will be taken before and after the addition of ozone. Samples will be analyzed using GC/MS/FID. |
UMBS PROPHET Tower | |
| The Effects of Selective Tree Species Girdling on Breeding Bird Species in an Aspen-Dominated Forest: A Preliminary Assessment |
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| Freshwater Advanced Aquatic Sensor Workshop: Sensors, Platforms and Data Management |
Aquatic sensor technology is developing rapidly, yet mechanisms and opportunities for limnologists and field biologists to receive training in these new technologies are limited. This workshop will address critical aspects of the sensor lifecyle, including: * Sensor selection, deployment and maintainance |
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| Dynamics of nitrogen oxides and ozone above and within a mixed hardwood forest in northern Michigan |
The dynamic behavior of nitrogen oxides (NO + NO2 = NOx) and ozone (O3) above and within the canopy at the University of Michigan Biological Station AmeriFlux tower was investigated during the summer and the fall of 2008. A daily maximum in nitric oxide (NO) levels was consistently observed during the morning hours between 6 and 9 AM EST above the canopy. The daily NO maximum ranged between 0.2 and 2 ppbv (with a median of 0.3 ppbv), which was 2 to 20 times above its atmospheric background. The sources and causes of this NO maximum were evaluated using NOx and O3 measurements and synoptic and micrometeorological data, which were supported by numerical simulations with a multi-layer canopy exchange model implemented in a single-column chemistry-climate model. The data indicated that the morning NO maximum was caused by the photolysis of NOx from non-local air masses, which were transported into the canopy from aloft during the morning breakup of the nocturnal boundary layer. Analysis of the multi-layer canopy model process tendencies indicated that this downward turbulent transport into the canopy compensated for the removal of NOx through chemistry and dry deposition. The latter process with turbulence appeared to drive the changes in crown layer NOx concentrations shortly after sunrise, in which the chemical sink was more significant. However, NOx dry deposition seemed to dominate NOx destruction throughout the day in the crown-layer as well as in the understory. We have conducted a number of simulations to assess the sensitivity of NOx and O3 concentrations on poorly constrained soil and foliage NOx emissions. Uncertainties associated with the emissions of NOx from the soil or from leaf-surface nitrate photolysis did not appear to explain the observed diurnal behavior in NOx (and O3) and, in particular the morning NOx peak concentration. However, consideration of the existence of an NO2 compensation point showed a maximum increase in early morning NOx and NO concentrations by about 30%. This highlighted the potential importance of leaf-level bi-directional exchange of NOx in determining the observed temporal variability in NOx at sites such as UMBS and the need for more detailed measurements of leaf-level NOx exchange. |
UMBS AmeriFlux Tower |