Science PI: James Washburne
Education CoI: Cyndy Henzel
Department of Hydrology and Water Resources
University of Arizona
Tucson, AZ 85721-0011
Duration: May 1, 1998-Apr. 30, 2002
Dr. Eric Layman of NASA's Marshall Research Center established the original GLOBE soil moisture protocol in 1995, consisting of daily observations of column soil moisture (at 10, 30, 60 and 90 cm) using gypsum blocks calibrated in situ against gravimetric measurements at 30 cm. The original protocol was deemed advanced and relatively expensive (~$400) which precluded most early GLOBE schools from even considering it. Calibration of the gypsum blocks has proven particularly daunting because multiple (20) calibration/meter pairs of measurements must be made over one or two complete drying cycles, which might span two months of time. In fact, soil moisture conditions at most GLOBE sites during the school year (which happen to be in relative humid zones of the United States) rarely dry to the point where the gypsum blocks exhibit much sensitivity to the relatively moist soil moisture conditions. Further, gypsum blocks slowly degrade, particularly in acidic and moist soils, which necessitates annual replacement and recalibration. Never-the-less, gypsum blocks have given several schools the opportunity to monitor short-term soil moisture variations at multiple soil levels over an extended period of time and enhance our knowledge of regional and seasonal soil moisture variability.
The science/education team of Dr. Jim Washburne and Cyndy Henzel of the Department of Hydrology and Water Resources at the University of Arizona were selected by NSF in the spring of 1995 to follow this initial phase of GLOBE. Our initial emphasis was to modify the protocol for accessibility by all students, develop learning activities that supported the protocol and work collaboratively with the Soil Characterization investigation. There were two serious issues that had to be addressed. First, the soil auger is unmanageable by most younger students and fairly expensive. Second, gravimetric sampling is destructive in that repeated sampling of the same point alters soil characteristics and invalidates the measurement. Thus, three new gravimetric sampling patterns were introduced in the 1996 TeacherÆs Guide to give students and schools a range of progressively more difficult sampling options. They were the near-surface ôStarö pattern, the 50 m transect, and the depth profile ôStarö pattern, where the ôStarö pattern simply allows the school to locate and cluster their observations without resampling the same point. Students collect samples using either a soil auger or alternatively, a shovel or trowel. A monthly interval was selected to capture the basic seasonality of the variation. Near-surface observations were made in the open at 5 and 10 cm to better support potential comparisons with microwave simulations or observations. The gypsum block technique was designated an optional protocol. The learning activities "The data gameö, ôSoils in your backyardö, ôDigging aroundö, ôSoils and spongesö and ôThe great decomposerö were developed in conjunction with the Soil Characterization team. We led the initiative to gather more site metadata but the lack of effective outreach and follow-up training of GLOBE teachers has limited this effort.
The soil moisture protocols were refined further and extended for the 1997 TeacherÆs Guide. Analysis of preliminary GLOBE data indicated that soil moisture variability is greatest (and most interesting) during transitions from generally dry periods (summers) to generally wet periods (winters). The sampling frequency and duration were modified to better capture this variation by making 12 measurements at a regular interval (determined by the school) during such transitional periods. This sampling should fit better into the traditional model of thematic units of limited duration. Another limitation for many schools was the lack of adequate soil drying facilities. A microwave and low temperature drying option were developed to alleviate this problem. Soil temperature (at 5 and 10 cm) and infiltration measurements were added to complement soil moisture data. A comprehensive framework was developed to align and focus learning activities with specific protocols. In general, we believe that the science protocols are supported best when they are preceded by basic exploration and discovery activities and followed up with modeling and analysis activities with a strong emphasis on inquiry and experimental-based learning.
There are a number of educational objectives that this investigation strives to meet. These include mentoring of students by scientists, both in areas of scientific methodology and environmental awareness, modeling teaching behaviors and attitudes, and a systematic approach to learning and thinking. It takes a special and a strong commitment on our part to training, outreach and development of learning activities to meet these objectives.
Original Title: The importance of soil moisture to global climate change
Publications: Washburne, J.C., 1998, Preliminary analysis of GLOBE soil moisture data, Proc. Amer. Meteor. Soc., Special Session on Hydrology, 5 p.
Rahman, A.F., Washburne, J.C., Moran, M.S. and Batchily, K., 1997, Regional-scale surface flux estimation by combined use of remote sensing and meteorologic data, In Press: Rem. Sensing of the Environ..,
Washburne, J.C., 1997, Preliminary analysis of GLOBE soil moisture data, Second Annual GLOBE Conf., Airlie, VA, http://www hwr.arizona.edu/globe/sci/airlie97.html
Washburne, J.C., 1998, Preliminary analysis of GLOBE soil moisture data, Proc. Am. Meteor. Soc., 14th Conf. On Hydrology, 5 p.
Washburne, J., Yucel, I., and Shuttleworth, J. 1997, Model and observed surface water budgets over selected sites in North America, Proc. Am. Meteor. Soc., 13th Conf. On Hydrology, p. 198-199.