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• 1. [Article] Effect of temperature and tissue type on fatty acid signatures of two species of North Pacific juvenile gadids: A laboratory feeding study

  To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier ...

  Citation × Citation Citation Abstract Copy Title: Effect of temperature and tissue type on fatty acid signatures of two species of North Pacific juvenile gadids: A laboratory feeding study Author: Parrish, Christopher C., Laurel, Benjamin J., Copeman, Louise A. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/journal-of-experimental-marine-biology-and-ecology/. Title: Effect of temperature and tissue type on fatty acid signatures of two species of North Pacific juvenile gadids: A laboratory feeding study Author: Parrish, Christopher C., Laurel, Benjamin J., Copeman, Louise A. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/journal-of-experimental-marine-biology-and-ecology/. Close

• 2. [Article] CopemanLouiseHMSCEffectTemperatureTissue.pdf

  Citation × Citation Citation Abstract Copy Title: CopemanLouiseHMSCEffectTemperatureTissue.pdf Author: Parrish, Christopher C., Copeman, Louise A., Laurel, Benjamin J. Title: CopemanLouiseHMSCEffectTemperatureTissue.pdf Author: Parrish, Christopher C., Copeman, Louise A., Laurel, Benjamin J. Close

• 3. [Article] CopemanLouiseHMSCEffectTemperatureTissueSupplementalMaterial.pdf

  Citation × Citation Citation Abstract Copy Title: CopemanLouiseHMSCEffectTemperatureTissueSupplementalMaterial.pdf Author: Parrish, Christopher C., Laurel, Benjamin J., Copeman, Louise A. Title: CopemanLouiseHMSCEffectTemperatureTissueSupplementalMaterial.pdf Author: Parrish, Christopher C., Laurel, Benjamin J., Copeman, Louise A. Close

• 4. [Article] Grow Tubes Change Microclimate and Bush Architecture but Have Little Effect on Bush Biomass Allocation at the End of the Establishment Year in Blueberry

  To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the American ...

  Citation × Citation Citation Abstract Copy Title: Grow Tubes Change Microclimate and Bush Architecture but Have Little Effect on Bush Biomass Allocation at the End of the Establishment Year in Blueberry Author: Chaves, Bernardo, Tarara, Julie M., Strik, Bernadine C. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the American Society for Horticultural Science and can be found at: http://hortsci.ashspublications.org/. Title: Grow Tubes Change Microclimate and Bush Architecture but Have Little Effect on Bush Biomass Allocation at the End of the Establishment Year in Blueberry Author: Chaves, Bernardo, Tarara, Julie M., Strik, Bernadine C. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the American Society for Horticultural Science and can be found at: http://hortsci.ashspublications.org/. Close

• 5. [Article] Thermal effects of hydrothermal circulation and seamount subduction: Temperatures in the Nankai Trough Seismogenic Zone Experiment transect, Japan

  This is the publisher's version of record. The original submission is copyrighted by American Geophysical Union and can be found here: http://www.agu.org/

  Citation × Citation Citation Abstract Copy Title: Thermal effects of hydrothermal circulation and seamount subduction: Temperatures in the Nankai Trough Seismogenic Zone Experiment transect, Japan Author: Harris, R. N., Spinelli, G. A. This is the publisher's version of record. The original submission is copyrighted by American Geophysical Union and can be found here: http://www.agu.org/ Title: Thermal effects of hydrothermal circulation and seamount subduction: Temperatures in the Nankai Trough Seismogenic Zone Experiment transect, Japan Author: Harris, R. N., Spinelli, G. A. This is the publisher's version of record. The original submission is copyrighted by American Geophysical Union and can be found here: http://www.agu.org/ Close

• 6. [Article] Glacier changes and climate trends derived from multiple sources in the data scarce Cordillera Vilcanota region, southern Peruvian Andes

  This is the publisher’s final pdf. The published article is copyrighted by Copernicus Publications on behalf of the European Geosciences Union and can be found at: http://www.the-cryosphere.net/.

  Citation × Citation Citation Abstract Copy Title: Glacier changes and climate trends derived from multiple sources in the data scarce Cordillera Vilcanota region, southern Peruvian Andes Author: Silverio, W., Burns, Patrick J. (Patrick Joseph), Salzmann, N., Portocarrero, C., Huggel, C., Mark, B. G., Rohrer, M. This is the publisher’s final pdf. The published article is copyrighted by Copernicus Publications on behalf of the European Geosciences Union and can be found at: http://www.the-cryosphere.net/. Title: Glacier changes and climate trends derived from multiple sources in the data scarce Cordillera Vilcanota region, southern Peruvian Andes Author: Silverio, W., Burns, Patrick J. (Patrick Joseph), Salzmann, N., Portocarrero, C., Huggel, C., Mark, B. G., Rohrer, M. This is the publisher’s final pdf. The published article is copyrighted by Copernicus Publications on behalf of the European Geosciences Union and can be found at: http://www.the-cryosphere.net/. Close

• 7. [Article] Mixing Measurements on an Equatorial Ocean Mooring

  Vaned, internally recording instruments that measure temperature fluctuations using FP07 thermistors, including fluctuations in the turbulence wavenumber band, have been built, tested, and deployed on ...

  Citation × Citation Citation Abstract Copy Title: Mixing Measurements on an Equatorial Ocean Mooring Author: Moum, J. N., Nash, J. D. Vaned, internally recording instruments that measure temperature fluctuations using FP07 thermistors, including fluctuations in the turbulence wavenumber band, have been built, tested, and deployed on a Tropical Atmosphere Ocean (TAO) mooring at 0°, 140°W. These were supplemented with motion packages that measure linear accelerations, from which an assessment of cable displacement and speed was made. Motions due to vortex-induced vibrations caused by interaction of the mean flow with the cable are small (rms < 0.15 cable diameters) and unlikely to affect estimates of the temperature variance dissipation rate χ[subscript]T. Surface wave–induced cable motions are significant, commonly resulting in vertical displacements of ±1 m and vertical speeds of ±0.5 m s⁻¹ on 2–10-s periods. These motions produce an enhancement to the measurement of temperature gradient in the surface wave band herein that is equal to the product of the vertical cable speed and the vertical temperature gradient (i.e., dT/dt ~w[subscript]cdT/dz). However, the temperature gradient spectrum is largely unaltered at higher and lower frequencies; in particular, there exists a clear scale separation between frequencies contaminated by surface waves and the turbulence subrange. The effect of cable motions on spectral estimates of χ[subscript]T is evaluated and determined to result in acceptably small uncertainties (< a factor of two 95% of the time, based on 60-s averages). Time series of χT and the inferred turbulent kinetic energy dissipation rate ϵ are consistent with historical data from the same equatorial location. Title: Mixing Measurements on an Equatorial Ocean Mooring Author: Moum, J. N., Nash, J. D. Vaned, internally recording instruments that measure temperature fluctuations using FP07 thermistors, including fluctuations in the turbulence wavenumber band, have been built, tested, and deployed on a Tropical Atmosphere Ocean (TAO) mooring at 0°, 140°W. These were supplemented with motion packages that measure linear accelerations, from which an assessment of cable displacement and speed was made. Motions due to vortex-induced vibrations caused by interaction of the mean flow with the cable are small (rms < 0.15 cable diameters) and unlikely to affect estimates of the temperature variance dissipation rate χ[subscript]T. Surface wave–induced cable motions are significant, commonly resulting in vertical displacements of ±1 m and vertical speeds of ±0.5 m s⁻¹ on 2–10-s periods. These motions produce an enhancement to the measurement of temperature gradient in the surface wave band herein that is equal to the product of the vertical cable speed and the vertical temperature gradient (i.e., dT/dt ~w[subscript]cdT/dz). However, the temperature gradient spectrum is largely unaltered at higher and lower frequencies; in particular, there exists a clear scale separation between frequencies contaminated by surface waves and the turbulence subrange. The effect of cable motions on spectral estimates of χ[subscript]T is evaluated and determined to result in acceptably small uncertainties (< a factor of two 95% of the time, based on 60-s averages). Time series of χT and the inferred turbulent kinetic energy dissipation rate ϵ are consistent with historical data from the same equatorial location. Close

• 8. [Article] Effects of mesoscale processes on phytoplankton chlorophyll off Baja California

  This is the publisher’s final pdf. The published article is copyrighted by American Geophysical Union and can be found at: http://sites.agu.org/.

  Citation × Citation Citation Abstract Copy Title: Effects of mesoscale processes on phytoplankton chlorophyll off Baja California Author: Gaxiola-Castro, Gilberto, Strub, P. Ted, T. Leticia Espinosa-Carreon, T. Leticia, Beier, Emilio, Kurczyn, J. A. This is the publisher’s final pdf. The published article is copyrighted by American Geophysical Union and can be found at: http://sites.agu.org/. Title: Effects of mesoscale processes on phytoplankton chlorophyll off Baja California Author: Gaxiola-Castro, Gilberto, Strub, P. Ted, T. Leticia Espinosa-Carreon, T. Leticia, Beier, Emilio, Kurczyn, J. A. This is the publisher’s final pdf. The published article is copyrighted by American Geophysical Union and can be found at: http://sites.agu.org/. Close

• 9. [Article] Inertial-Convective Subrange Estimates of Thermal Variance Dissipation Rate from Moored Temperature Measurements

  A procedure for estimating thermal variance dissipation rate χ[subscript]T by scaling the inertial-convective subrange of temperature gradient spectra from thermistor measurements on a Tropical Atmosphere ...

  Citation × Citation Citation Abstract Copy Title: Inertial-Convective Subrange Estimates of Thermal Variance Dissipation Rate from Moored Temperature Measurements Author: Zhang, Yanwei, Moum, James N. A procedure for estimating thermal variance dissipation rate χ[subscript]T by scaling the inertial-convective subrange of temperature gradient spectra from thermistor measurements on a Tropical Atmosphere Ocean (TAO) equatorial mooring, maintained by NOAA’s National Data Buoy Center, is demonstrated. The inertial-convective subrange of wavenumbers/frequencies is contaminated by the vertical motion induced by the pumping of the surface float by surface gravity waves through the local vertical temperature gradient. The uncontaminated signal can be retrieved by removing the part of the measured signal that is coherent with the signal induced by surface gravity waves, which must be measured independently. An estimate of χ[subscript]T is then obtained by fitting corrected spectra to theoretical temperature gradient spectra over the inertial-convective subrange (0.05 < ƒ < 0.5 Hz); this estimate is referred to as χ[subscript]T[superscript]IC. Here χ[subscript]T[superscript]IC was calculated over 120-min intervals and compared with estimates of χ[subscript]T[superscript]o determined by scaling temperature gradient spectra at high wavenumbers (viscous-convective and viscous-diffusive subranges). Large differences up to a factor of 20 and of unknown origin occur infrequently, especially when both background currents and vertical temperature gradients are weak, but the results herein indicate that 75% of the data pairs are within a factor of 3 of each other. Tests on 15-, 30-, 60-, 120-min intervals demonstrate that differences between the two methods are nearly random, unbiased, and less than estimates of natural variability determined from unrelated experiments at the same location. Because the inertial-convective subrange occupies a lower-frequency range than is typically used for turbulence measurements, the potential for more routine measurements of χ[subscript]T exists. The evaluation of degraded signals (resampled from original measurements) indicates that a particularly important component of such a measurement is the independent resolution of the surface wave–induced signal. Title: Inertial-Convective Subrange Estimates of Thermal Variance Dissipation Rate from Moored Temperature Measurements Author: Zhang, Yanwei, Moum, James N. A procedure for estimating thermal variance dissipation rate χ[subscript]T by scaling the inertial-convective subrange of temperature gradient spectra from thermistor measurements on a Tropical Atmosphere Ocean (TAO) equatorial mooring, maintained by NOAA’s National Data Buoy Center, is demonstrated. The inertial-convective subrange of wavenumbers/frequencies is contaminated by the vertical motion induced by the pumping of the surface float by surface gravity waves through the local vertical temperature gradient. The uncontaminated signal can be retrieved by removing the part of the measured signal that is coherent with the signal induced by surface gravity waves, which must be measured independently. An estimate of χ[subscript]T is then obtained by fitting corrected spectra to theoretical temperature gradient spectra over the inertial-convective subrange (0.05 < ƒ < 0.5 Hz); this estimate is referred to as χ[subscript]T[superscript]IC. Here χ[subscript]T[superscript]IC was calculated over 120-min intervals and compared with estimates of χ[subscript]T[superscript]o determined by scaling temperature gradient spectra at high wavenumbers (viscous-convective and viscous-diffusive subranges). Large differences up to a factor of 20 and of unknown origin occur infrequently, especially when both background currents and vertical temperature gradients are weak, but the results herein indicate that 75% of the data pairs are within a factor of 3 of each other. Tests on 15-, 30-, 60-, 120-min intervals demonstrate that differences between the two methods are nearly random, unbiased, and less than estimates of natural variability determined from unrelated experiments at the same location. Because the inertial-convective subrange occupies a lower-frequency range than is typically used for turbulence measurements, the potential for more routine measurements of χ[subscript]T exists. The evaluation of degraded signals (resampled from original measurements) indicates that a particularly important component of such a measurement is the independent resolution of the surface wave–induced signal. Close

• 10. [Article] Kelvin waves in stratospheric temperature observed by the Microwave Limb Sounder

  The three-dimensional (3-D) structure of stratospheric Kelvin waves is revealed using data from the Microwave Limb Sounder for the period July 1992 to April 1993. Four Kelvin wave modes are identified, ...

  Citation × Citation Citation Abstract Copy Title: Kelvin waves in stratospheric temperature observed by the Microwave Limb Sounder Author: Dunkerton, Timothy J., Wu, Dong, Mote, Philip W. The three-dimensional (3-D) structure of stratospheric Kelvin waves is revealed using data from the Microwave Limb Sounder for the period July 1992 to April 1993. Four Kelvin wave modes are identified, two for zonal wave number 1 (k = 1) and two for k = 2, using extended empirical orthogonal functions. The 3-D structures of the modes agree with linear theory and satisfy the dispersion relation for Kelvin waves, and with periods ranging from 4.5 to 10 days the modes mostly fall near the boundary between ‘‘fast’’ and ‘‘slow’’ Kelvin waves [Canziani et al., 1998]. The analysis also identifies a feature that may correspond with the ‘‘pancake structures’’ associated with inertial instability. Title: Kelvin waves in stratospheric temperature observed by the Microwave Limb Sounder Author: Dunkerton, Timothy J., Wu, Dong, Mote, Philip W. The three-dimensional (3-D) structure of stratospheric Kelvin waves is revealed using data from the Microwave Limb Sounder for the period July 1992 to April 1993. Four Kelvin wave modes are identified, two for zonal wave number 1 (k = 1) and two for k = 2, using extended empirical orthogonal functions. The 3-D structures of the modes agree with linear theory and satisfy the dispersion relation for Kelvin waves, and with periods ranging from 4.5 to 10 days the modes mostly fall near the boundary between ‘‘fast’’ and ‘‘slow’’ Kelvin waves [Canziani et al., 1998]. The analysis also identifies a feature that may correspond with the ‘‘pancake structures’’ associated with inertial instability. Close