Welcome to the Berkeley Biometeorology Lab Web site.
We are in the process of upgrading the web site so please bear with us and feel free to send me an email if you find any bugs:
jverfail at berkeley.edu
Biometeorology is a field that explores the interactions between life and its surrounding environment. Biometeorology is instrumental in providing information that is of use to biogeoscientists, atmospheric scientists, remote sensing scientists, hydrologists and ecologists working on problems of the carbon, water, and nitrogen cycles and on the prediction of weather and climate, the chemical state of the atmosphere and the structure, function and dynamics of ecosystems—most of these problems rely on quantifying and predicting the state of the environment of the air, leaves and soil and fluxes of trace gases and energy between vegetated canopies and the atmosphere—and biometeorology provides the science for measuring and modeling those fluxes and states. Stated otherwise, predictions stemming from biogeoscience models are most accurate when they consider biometeorological theory and translate governing weather information of the region to the state or condition of the leaf and soil.
Our research program focuses on studying: ‘the physical, biological and chemical processes that govern trace gas and energy exchange between the terrestrial biosphere and the atmosphere’. In layman terms, our broad objective is to understand how the terrestrial biosphere ‘breathes’; plants and microbes exchange trace gases, in and out of the atmosphere, in their quest to acquire the energy needed to support their metabolism.
The science of biometeorology requires the study of complexity, defined as the study of systems whose whole is a function of many inter-connected parts. One of the tasks of biometeorology is to interpret a suite non-linear and coupled information from an array of biophysical processes (e.g. turbulence and diffusion, photon transfer through vegetation, evaporation, photosynthesis, plant and soil respiration, and stomatal mechanics) that span a spectrum of time and space scales. The time scales of my research spans events occurring on periods of seconds, hours, days, seasons, years and decades. The spatial scales of my work differ vertically and horizontally. The vertical dimensions of our work spans the scales associated with soil profile (-1 m), plant canopy (10+ m) and the planetary boundary layer (1000+ m). The horizontal dimensions of our work span the scales of a leaf (0.1 m), the fetch across a landscape (100 - 1000 m), and the continent and globe (1000-10,000 km).
Our research approach involves the coordinated use of experimental measurements and theoretical models to understand the physical, biological, and chemical processes that control trace gas fluxes between the biosphere and atmosphere and to quantify their temporal and spatial variations. The spatial scales of this work ranges from the dimension of a leaf through the depth of plant canopies and the planetary boundary layer and the horizontal extent of landscapes. The temporal aspect of this work ranges from seconds through hours, days, seasons and years.
Measuring and modeling carbon, water and energy exchange of ecosystems that experience extremes in water is the focus of our current research activities. One set of studies is being conducted over semi-arid, Mediterranean oak woodlands and annual grasslands, which access deep water tables. Another set of studies is being conducted over seasonally flooded peatlands and rice paddies, with access to shallow water tables. The upscaling this information regionally and globally is being accomplished through our coordination and association with the FLUXNET project and concurrent acquisition of multi-faceted remote sensing products.
Last Updated: 2013-10-02
This material is based upon work supported by the National Science Foundation and US Department of Energy. Any opinions, findings, conclusions, or recommendations expressed in the material are those of the author(s) and do not necessarily reflect the views of the supporters.