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• 1. [Article] Hydrological characteristics of recurrent slope lineae on Mars: Evidence for liquid flow through regolith and comparisons with Antarctic terrestrial analogs

  This is the author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/icarus/.

  Citation × Citation Citation Abstract Copy Title: Hydrological characteristics of recurrent slope lineae on Mars: Evidence for liquid flow through regolith and comparisons with Antarctic terrestrial analogs Author: Levy, Joseph This is the author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/icarus/. Title: Hydrological characteristics of recurrent slope lineae on Mars: Evidence for liquid flow through regolith and comparisons with Antarctic terrestrial analogs Author: Levy, Joseph This is the author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/icarus/. Close

• 2. [Article] Estimates of the 10-m Neutral Sea Surface Drag Coefficient from Aircraft Eddy-Covariance Measurements

  This is the publisher’s final pdf. The published article is copyrighted by the American Meteorological Society and can be found at: http://journals.ametsoc.org/loi/phoc.

  Citation × Citation Citation Abstract Copy Title: Estimates of the 10-m Neutral Sea Surface Drag Coefficient from Aircraft Eddy-Covariance Measurements Author: Andreas, Edgar L., Vickers, Dean, Mahrt, Larry This is the publisher’s final pdf. The published article is copyrighted by the American Meteorological Society and can be found at: http://journals.ametsoc.org/loi/phoc. Title: Estimates of the 10-m Neutral Sea Surface Drag Coefficient from Aircraft Eddy-Covariance Measurements Author: Andreas, Edgar L., Vickers, Dean, Mahrt, Larry This is the publisher’s final pdf. The published article is copyrighted by the American Meteorological Society and can be found at: http://journals.ametsoc.org/loi/phoc. Close

• 3. [Article] Surface Wave Effects on High-Frequency Currents over a Shelf Edge Bank

  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: Surface Wave Effects on High-Frequency Currents over a Shelf Edge Bank Author: Teague, W. J., Moum, J. N., Wijesekera, H. W., Fribance, D. B., Rogers, W. E., Wang, D. W., Jarosz, E. 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 Meteorological Society and can be found at: http://journals.ametsoc.org/loi/phoc. Title: Surface Wave Effects on High-Frequency Currents over a Shelf Edge Bank Author: Teague, W. J., Moum, J. N., Wijesekera, H. W., Fribance, D. B., Rogers, W. E., Wang, D. W., Jarosz, E. 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 Meteorological Society and can be found at: http://journals.ametsoc.org/loi/phoc. Close

• 4. [Article] Quantifying the length-scale dependence of surf zone advection

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

  Citation × Citation Citation Abstract Copy Title: Quantifying the length-scale dependence of surf zone advection Author: Wilson, Greg W., Oezkan-Haller, H. Tuba, Holman, Robert A. This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical Union and can be found at: http://www.agu.org/journals/jgr/. Title: Quantifying the length-scale dependence of surf zone advection Author: Wilson, Greg W., Oezkan-Haller, H. Tuba, Holman, Robert A. This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical Union and can be found at: http://www.agu.org/journals/jgr/. Close

• 5. [Article] Heat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, Japan

  [1] We report detailed thermal measurements undertaken during Integrated Ocean Drilling Program (IODP) Expeditions 315 and 316 along the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) transect offshore ...

  Citation × Citation Citation Abstract Copy Title: Heat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, Japan Author: Schmidt‐Schierhorn, Friederike, Spinelli, Glenn, Harris, Robert N. [1] We report detailed thermal measurements undertaken during Integrated Ocean Drilling Program (IODP) Expeditions 315 and 316 along the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) transect offshore the Kii Peninsula, Japan. Geothermal objectives included determining thermophysical rock properties of the cored material and characterizing the background thermal regime along this transect. New thermal conductivity measurements made with a divided bar are reported and supplement shipboard full‐ and half‐space thermal conductivity measurements for a total of 938 thermal conductivity measurements. Thermal conductivity varies between about 1.0 W m⁻¹ K⁻¹ near the seafloor to 1.6 W m⁻¹ K⁻¹ at a depth of 1 km. Thermal conductivity generally increases with depth and correlates with variations in porosity and lithology. Thermal gradients along the transect are characterized by 48 sediment temperature measurements from 6 sites. Thermal corrections for the effects of bathymetric relief and sedimentation improve the confidence with which the heat flow values can be interpreted. Heat flow generally decreases with landward distance from the deformation front and varies from 70 mW m⁻² just landward of the deformation front to 54 mW m⁻² at sites characterizing the outer fore‐arc high and to 57 mW m⁻² at the Kumano Basin Site. IODP heat flow measurements are significantly lower than nearby seafloor heat flow measurements. This difference is most likely due to variations in bottom water temperature that have a large effect on values of seafloor heat flow. Thus the heat flow of the Nankai accretionary prism is lower than previously thought. We present thermal models of subduction along this transect and explore the impact of the initial geotherm. Conductive plate cooling based on the age of subducting seafloor (20 Myr) under predicts the observed heat flow. We find a good fit to the data using a geotherm appropriate for 10 Myr seafloor. The extra heat is interpreted in terms of back‐arc thermal environments. Title: Heat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, Japan Author: Schmidt‐Schierhorn, Friederike, Spinelli, Glenn, Harris, Robert N. [1] We report detailed thermal measurements undertaken during Integrated Ocean Drilling Program (IODP) Expeditions 315 and 316 along the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) transect offshore the Kii Peninsula, Japan. Geothermal objectives included determining thermophysical rock properties of the cored material and characterizing the background thermal regime along this transect. New thermal conductivity measurements made with a divided bar are reported and supplement shipboard full‐ and half‐space thermal conductivity measurements for a total of 938 thermal conductivity measurements. Thermal conductivity varies between about 1.0 W m⁻¹ K⁻¹ near the seafloor to 1.6 W m⁻¹ K⁻¹ at a depth of 1 km. Thermal conductivity generally increases with depth and correlates with variations in porosity and lithology. Thermal gradients along the transect are characterized by 48 sediment temperature measurements from 6 sites. Thermal corrections for the effects of bathymetric relief and sedimentation improve the confidence with which the heat flow values can be interpreted. Heat flow generally decreases with landward distance from the deformation front and varies from 70 mW m⁻² just landward of the deformation front to 54 mW m⁻² at sites characterizing the outer fore‐arc high and to 57 mW m⁻² at the Kumano Basin Site. IODP heat flow measurements are significantly lower than nearby seafloor heat flow measurements. This difference is most likely due to variations in bottom water temperature that have a large effect on values of seafloor heat flow. Thus the heat flow of the Nankai accretionary prism is lower than previously thought. We present thermal models of subduction along this transect and explore the impact of the initial geotherm. Conductive plate cooling based on the age of subducting seafloor (20 Myr) under predicts the observed heat flow. We find a good fit to the data using a geotherm appropriate for 10 Myr seafloor. The extra heat is interpreted in terms of back‐arc thermal environments. Close

• 6. [Article] Shelfbreak upwelling induced by alongshore currents: analytical and numerical results

  This is the publisher's version of record. The original submission is copyrighted by Cambridge University Press and can be found here: http://www.tos.org/

  Citation × Citation Citation Abstract Copy Title: Shelfbreak upwelling induced by alongshore currents: analytical and numerical results Author: Palma, Elbio D., Miller, Robert N., Matano, Ricardo P. This is the publisher's version of record. The original submission is copyrighted by Cambridge University Press and can be found here: http://www.tos.org/ Title: Shelfbreak upwelling induced by alongshore currents: analytical and numerical results Author: Palma, Elbio D., Miller, Robert N., Matano, Ricardo P. This is the publisher's version of record. The original submission is copyrighted by Cambridge University Press and can be found here: http://www.tos.org/ Close

• 7. [Article] Turbulent Kinetic Energy Dissipation in Barrow Canyon

  This is the publisher’s final pdf. The published article is copyrighted by the American Meteorological Society and can be found at: http://www.ametsoc.org/pubs/journals/jpo/index.html.

  Citation × Citation Citation Abstract Copy Title: Turbulent Kinetic Energy Dissipation in Barrow Canyon Author: Shroyer, E. L. This is the publisher’s final pdf. The published article is copyrighted by the American Meteorological Society and can be found at: http://www.ametsoc.org/pubs/journals/jpo/index.html. Title: Turbulent Kinetic Energy Dissipation in Barrow Canyon Author: Shroyer, E. L. This is the publisher’s final pdf. The published article is copyrighted by the American Meteorological Society and can be found at: http://www.ametsoc.org/pubs/journals/jpo/index.html. Close

• 8. [Article] The Direct Breaking of Internal Waves at Steep Topography

  This is the publisher’s final pdf. The published article is copyrighted by The Oceanography Society, and can be found at: http://www.tos.org/oceanography/.

  Citation × Citation Citation Abstract Copy Title: The Direct Breaking of Internal Waves at Steep Topography Author: Pinkel, Robert, Buijsman, Maarten, Klymak, Jody M., Nash, Jonathan D., Legg, Sonya, Alford, Matthew H. This is the publisher’s final pdf. The published article is copyrighted by The Oceanography Society, and can be found at: http://www.tos.org/oceanography/. Title: The Direct Breaking of Internal Waves at Steep Topography Author: Pinkel, Robert, Buijsman, Maarten, Klymak, Jody M., Nash, Jonathan D., Legg, Sonya, Alford, Matthew H. This is the publisher’s final pdf. The published article is copyrighted by The Oceanography Society, and can be found at: http://www.tos.org/oceanography/. Close

• 9. [Article] International Mekong River Basin: Events, Conflicts or Cooperation, and Policy Implications

  “International river basin is defined as an area extending over two or more states determined by the watershed limits of the system of waters, including surface and underground waters, flowing into a ...

  Citation × Citation Citation Abstract Copy Title: International Mekong River Basin: Events, Conflicts or Cooperation, and Policy Implications Author: Yorth, Bunny “International river basin is defined as an area extending over two or more states determined by the watershed limits of the system of waters, including surface and underground waters, flowing into a common terminus” (Shapiro-Libai, 1969, p. 22). There are 276 international river basins providing almost 60% of global freshwater and supporting at least 40% of the world population. Over recent decades, the riparian governments of the Lancang-Mekong River, like other international river basin leaders, may have had different and sometimes conflicting interests in promoting their economies through exploiting shared water, preserving their aquatic resources, or both, in the basin. Accordingly, their interactions have created water events, which can be neutral, conflictive, or cooperative. In this secondary-data paper, there are seven levels of conflicts and seven levels of cooperation, ranging from -7 to -1 and from +1 to +7, respectively. The main discussions of this paper focus on frequencies in each level, outstanding factors found in either conflicts or cooperation of the events, and policy implications. The 190 events from 1952 to 2010 in the Lancang-Mekong River Basin are found to be overwhelmingly cooperative. The result means that six riparian governments – China, Burma, Laos, Thailand, Cambodia, and Vietnam – would like to work together. However, these nations will need to do more, especially relating to three outstanding factors found in the conflictive events: dam development, navigation projects, and droughts. In addition, memberships of both China and Burma are strongly needed in the Mekong River Committee (MRC). Title: International Mekong River Basin: Events, Conflicts or Cooperation, and Policy Implications Author: Yorth, Bunny “International river basin is defined as an area extending over two or more states determined by the watershed limits of the system of waters, including surface and underground waters, flowing into a common terminus” (Shapiro-Libai, 1969, p. 22). There are 276 international river basins providing almost 60% of global freshwater and supporting at least 40% of the world population. Over recent decades, the riparian governments of the Lancang-Mekong River, like other international river basin leaders, may have had different and sometimes conflicting interests in promoting their economies through exploiting shared water, preserving their aquatic resources, or both, in the basin. Accordingly, their interactions have created water events, which can be neutral, conflictive, or cooperative. In this secondary-data paper, there are seven levels of conflicts and seven levels of cooperation, ranging from -7 to -1 and from +1 to +7, respectively. The main discussions of this paper focus on frequencies in each level, outstanding factors found in either conflicts or cooperation of the events, and policy implications. The 190 events from 1952 to 2010 in the Lancang-Mekong River Basin are found to be overwhelmingly cooperative. The result means that six riparian governments – China, Burma, Laos, Thailand, Cambodia, and Vietnam – would like to work together. However, these nations will need to do more, especially relating to three outstanding factors found in the conflictive events: dam development, navigation projects, and droughts. In addition, memberships of both China and Burma are strongly needed in the Mekong River Committee (MRC). Close

• 10. [Article] Analysis of the present and future winter Pacific-North American teleconnection in the ECHAM5 global and RegCM3 regional climate models

  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 Springer ...

  Citation × Citation Citation Abstract Copy Title: Analysis of the present and future winter Pacific-North American teleconnection in the ECHAM5 global and RegCM3 regional climate models Author: Allan, Andrea M., Hostetler, Steven W., Alder, Jay R. 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 Springer and can be found at: http://link.springer.com/journal/382. Title: Analysis of the present and future winter Pacific-North American teleconnection in the ECHAM5 global and RegCM3 regional climate models Author: Allan, Andrea M., Hostetler, Steven W., Alder, Jay R. 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 Springer and can be found at: http://link.springer.com/journal/382. Close