Index Catalog // ScholarsArchive@OSU

Turbulent supply of nutrients to phytoplankton at the New England shelf break front

Creator:: Hales, Burke, Hebert, Dave, and Marra, John
Abstract:: We present observations from deployments of a microstructure turbulence instrument (the Towed Microstructure and Auxiliary Sensor Instrument) aboard a pumping profiling vehicle (the Lamont Pumping SeaSoar) towed behind a research vessel at the New England shelf break front in August 2002. From these we determined coincident fine-scale vertical eddy diffusivity...
Resource Type:: Article
Full Text:: phytoplankton at the New England shelf break front, J. Geophys. Res., 114, C05010, doi:10.1029/2008JC005011. 1

A new mechanism for Dansgaard-Oeschger cycles

Creator:: Petersen, S. V., Schrag, D. P., and Clark, P. U.
Abstract:: We present a new hypothesis to explain the millennial-scale temperature variability recorded in ice cores known as Dansgaard-Oeschger (DO) cycles. We propose that an ice shelf acted in concert with sea ice to set the slow and fast timescales of the DO cycle, respectively. The abrupt warming at the onset...
Resource Type:: Article
Full Text:: , Paleoceanography, 28, 24–30, doi:10.1029/2012PA002364. 1. Introduction [2] During the last glacial period, the

Analytical solution and simplified analysis of coupled parent-daughter steady-state transport with multirate mass transfer

Creator:: Haggerty, Roy
Abstract:: In this technical note, a steady-state analytical solution of concentrations of a parent solute reacting to a daughter solute, both of which are undergoing transport and multirate mass transfer, is presented. Although the governing equations are complicated, the resulting solution can be expressed in simple terms. A function of the...
Resource Type:: Article
Full Text:: Resour. Res. 49, doi:10.1029/2012WR012821. 1. Introduction [2] Reactive or decaying solutes in the

A-posteriori analysis of surface energy budget closure to determine missed energy pathways

Creator:: Higgins, Chad W.
Abstract:: The residual of the surface energy budget is represented as the linearized sum of energy losses due to storage, advection and flux underestimation. Individual contributions to the residual can be quantified through constrained multiple linear regression which identifies the site specific processes that are responsible for the lack of energy...
Resource Type:: Article
Full Text:: . Lett., 39, L19403, doi:10.1029/2012GL052918. 1. Introduction [2] Measurements of the Earth’s surface

Storm-induced upwelling of high pCO2 waters onto the continental shelf of the western Arctic Ocean and implications for carbonate mineral saturation states

Creator:: Mathis, Jeremy T., Pickart, Robert S., Byrne, Robert H., McNeil, Craig L., Moore, G. W. K., Juranek, Laurie W., Liu, Xuewu, Ma, Jian, Easley, Regina A., Elliot, Matthew M., Cross, Jessica N., Reisdorph, Stacey C., Bahr, Frank, Morison, Jamie, and Lichendorf, Trina
Abstract:: The carbon system of the western Arctic Ocean is undergoing a rapid transition as sea ice extent and thickness decline. These processes are dynamically forcing the region, with unknown consequences for CO2 fluxes and carbonate mineral saturation states, particularly in the coastal regions where sensitive ecosystems are already under threat...
Resource Type:: Article
Full Text:: :10.1029/ 2012GL051574. 1. Introduction [2] The continental shelves of the western Arctic Ocean play an

The paradox of cooling streams in a warming world:Regional climate trends do not parallel variable local trends in stream temperature in the Pacific continental United States

Creator:: Arismendi, Ivan, Johnson, Sherri L., Dunham, Jason B., Haggerty, Roy, and Hockman-Wert, David
Abstract:: Temperature is a fundamentally important driver of ecosystem processes in streams. Recent warming of terrestrial climates around the globe has motivated concern about consequent increases in stream temperature. More specifically, observed trends of increasing air temperature and declining stream flow are widely believed to result in corresponding increases in stream...
Resource Type:: Article
Full Text:: :10.1029/2012GL051448. 1. Introduction [2] Temperature is a fundamental driver of processes affect- ing

Global net community production and the putative net heterotrophy of the oligotrophic oceans

Creator:: Westberry, Toby K., Williams, Peter J. le B., and Behrenfeld, Michael J.
Abstract:: Reconciling rates of organic carbon export from the euphotic zone with the consumption of organic material in the dark ocean remains one of the major quantitative uncertainties of the ocean carbon cycle. Euphotic zone net community production (NCP) provides one broad constraint on export flux and potential carbon drawdown. However,...
Resource Type:: Article
Full Text:: the oligotrophic oceans, Global Biogeochem. Cycles, 26, GB4019, doi:10.1029/2011GB004094. 1

Fuel moisture influences on fire-altered carbon in masticated fuels: An experimental study

Creator:: Brewer, Nolan W., Smith, Alistair M. S., Hatten, Jeffery A., Higuera, Philip E., Hudak, Andrew T., Ottmar, Roger D., and Tinkham, Wade T.
Abstract:: Biomass burning is a significant contributor to atmospheric carbon emissions but may also provide an avenue in which fire-affected ecosystems can accumulate carbon over time, through the generation of highly resistant fire-altered carbon. Identifying how fuel moisture, and subsequent changes in the fire behavior, relates to the production of fire-altered...
Resource Type:: Article
Full Text:: experimental study, J. Geophys. Res. Biogeosci., 118, 30–40, doi: 10.1029/2012JG002079. 1. Introduction [2

Mesoscale biogeochemical responses to iron fertilization in the upper layers of the Southern Ocean Iron Experiment areas

Creator:: Hales, Burke and Takahashi, Taro
Abstract:: During the Southern Ocean Iron Experiment (SOFeX), January-February 2002, two iron fertilization experiments were conducted at the south (66.45°S, 171.8°W) and north (56.23°S, 172°W) patches. The south patch was replete with all macronutrients, whereas the north patch was nearly depleted of silicate. Using a towed water sampling/measurement system, high resolution...
Resource Type:: Article
Full Text:: ., 117, C01018, doi:10.1029/2011JC006956. 1. Introduction [2] Surface waters of the Southern Ocean have

Shearman_Lentz_JGR_2007.pdf

Creator:: Shearman, R. Kipp and Lentz, Steven J.
Abstract:: Current and hydrographic observations from the Coastal Mixing and Optics experiment moored array, deployed from August 1996 through June 1997, are used to describe the velocity variability and evaluate the dynamics of circulation over the New England shelf on timescales ranging from a few days to several months. Subtidal (days...
Full Text:: mean and subtidal flow on the New England shelf,’’ J. Geophys. Res., 112, C02015, doi:10.1029

ScholarsArchive@OSU

Turbulent supply of nutrients to phytoplankton at the New England shelf break front

A new mechanism for Dansgaard-Oeschger cycles

Analytical solution and simplified analysis of coupled parent-daughter steady-state transport with multirate mass transfer

A-posteriori analysis of surface energy budget closure to determine missed energy pathways

Storm-induced upwelling of high pCO2 waters onto the continental shelf of the western Arctic Ocean and implications for carbonate mineral saturation states

The paradox of cooling streams in a warming world:Regional climate trends do not parallel variable local trends in stream temperature in the Pacific continental United States

Global net community production and the putative net heterotrophy of the oligotrophic oceans

Fuel moisture influences on fire-altered carbon in masticated fuels: An experimental study

Mesoscale biogeochemical responses to iron fertilization in the upper layers of the Southern Ocean Iron Experiment areas

Shearman_Lentz_JGR_2007.pdf

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