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Showing papers by "Wade R. McGillis published in 2015"


Journal ArticleDOI
TL;DR: In this paper, the authors used a combination of potential evapotranspiration (PET) models, which assume non-water-limited substrate moisture conditions, and actual evapOTranspiration model, which account for water-limited substrates, to predict green roof evapotsranspiration from local climate conditions.

48 citations


Journal ArticleDOI
TL;DR: In this paper, the authors determined the rates and pathways that govern gas transport through a mixed sea ice cover, and showed that very little mixed-layer ventilation takes place via gas diffusion through columnar sea ice.
Abstract: Sea ice is a defining feature of the polar marine environment. It is a critical domain for marine biota and it regulates ocean-atmosphere exchange, including the exchange of greenhouse gases such as CO2 and CH4. In this study, we determined the rates and pathways that govern gas transport through a mixed sea ice cover. N2O, SF6, 3He, 4He, and Ne were used as gas tracers of the exchange processes that take place at the ice-water and air-water interfaces in a laboratory sea ice experiment. Observation of the changes in gas concentrations during freezing revealed that He is indeed more soluble in ice than in water; Ne is less soluble in ice, and the larger gases (N2O and SF6) are mostly excluded during the freezing process. Model estimates of gas diffusion through ice were calibrated using measurements of bulk gas content in ice cores, yielding gas transfer velocity through ice (kice) of ∼5 × 10−4 m d−1. In comparison, the effective air-sea gas transfer velocities (keff) ranged up to 0.33 m d−1 providing further evidence that very little mixed-layer ventilation takes place via gas diffusion through columnar sea ice. However, this ventilation is distinct from air-ice gas fluxes driven by sea ice biogeochemistry. The magnitude of keff showed a clear increasing trend with wind speed and current velocity beneath the ice, as well as the combination of the two. This result indicates that gas transfer cannot be uniquely predicted by wind speed alone in the presence of sea ice.

26 citations


Journal ArticleDOI
TL;DR: Diurnal variation of net community production (NEP) and net community calcification (NEC) were measured in coral reef and seagrass biomes during October 2012 in the lower Florida Keys using a mesocosm enclosure and the oxygen gradient flux technique.
Abstract: (1) Dalhousie University, Halifax, NS, Canada, (9) LDEO, Columbia University, New York, NY, United States, (2) U.S. Geological Survey, St. Petersburg, FL, United States, (3) College of Marine Science, University of South Florida, St. Petersburg, FL, United States, (4) Cooperative Institute for Marine and Atmospheric Studies, University of Miami, Miami, FL, United States, (5) NOAA Atlantic Oceanographic and Meteorological Laboratory, Miami, United States, (6) Marine Sciences, The University of Trinidad and Tobago, Trinidad and Tobago, (7) National Commission for Knowledge and Use of Biodiversity (CONABIO), Mexico, (8) UAV Collaborative, Moffett Field, CA, United States

21 citations



Journal ArticleDOI
TL;DR: In this article, the authors measured hydrology and carbon speciation in watersheds of southwest Haiti to quantify the amount of inorganic carbon transport and found that these watersheds have some of the highest DIC and alkalinity reported.

3 citations