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• 31. [Article] Findley Lake lysimeter leachate, precipitation inflow, outflow, and throughfall data, June 1973-January 1974

  Data on soil leachate at three sites and four depths, throughfall, precipitation, and lake inflow and outflow are presented in this report.

  Citation × Citation Citation Abstract Copy Title: Findley Lake lysimeter leachate, precipitation inflow, outflow, and throughfall data, June 1973-January 1974 Author: Minden, Ralph V., U.S. International Biological Program. Coniferous Forest Biome, University of Washington, Ugolini, Fiorenzo C. Data on soil leachate at three sites and four depths, throughfall, precipitation, and lake inflow and outflow are presented in this report. Title: Findley Lake lysimeter leachate, precipitation inflow, outflow, and throughfall data, June 1973-January 1974 Author: Minden, Ralph V., U.S. International Biological Program. Coniferous Forest Biome, University of Washington, Ugolini, Fiorenzo C. Data on soil leachate at three sites and four depths, throughfall, precipitation, and lake inflow and outflow are presented in this report. Close

• 32. [Article] Rainfall over coastal waters of the Pacific Northwest

  The objective of this study was to ascertain the magnitude and distribution of rainfall over coastal waters of the northwestern United States and to compare values with those at nearby land stations. Precipitation ...

  Citation × Citation Citation Abstract Copy Title: Rainfall over coastal waters of the Pacific Northwest Author: Reed, Ronald Keith The objective of this study was to ascertain the magnitude and distribution of rainfall over coastal waters of the northwestern United States and to compare values with those at nearby land stations. Precipitation was measured with gauges at Totem, rainfall amounts were assessed from weather reports at lightships off the coast, and precipitation frequencies at lightships and land stations were examined. Results from the three methods were quite consistent; precipitation. on at sea was only about one-third that at coastal land stations. These values are appreciably less than previous estimates of oceanic rainfall in this area, and they support the view that a significant horizontal gradient of precipitation may exist between the coast and open sea. Rainfall typically occurs both at sea and ashore on the same day, but it rains fewer hours at sea. The relative amount of rain at sea varies with the type of atmospheric system, and rainfall at the coast appears to be intensified by frictional processes. Estimates of evaporation minus precipitation are less negative than earlier ones; consideration of their relation to surface salinity leads to distributions that are in good agreement with oceanographic knowledge. The newer values suggest that in this region the heat gain by the atmosphere may be less (but moisture entrainment may be greater) than was thought. Title: Rainfall over coastal waters of the Pacific Northwest Author: Reed, Ronald Keith The objective of this study was to ascertain the magnitude and distribution of rainfall over coastal waters of the northwestern United States and to compare values with those at nearby land stations. Precipitation was measured with gauges at Totem, rainfall amounts were assessed from weather reports at lightships off the coast, and precipitation frequencies at lightships and land stations were examined. Results from the three methods were quite consistent; precipitation. on at sea was only about one-third that at coastal land stations. These values are appreciably less than previous estimates of oceanic rainfall in this area, and they support the view that a significant horizontal gradient of precipitation may exist between the coast and open sea. Rainfall typically occurs both at sea and ashore on the same day, but it rains fewer hours at sea. The relative amount of rain at sea varies with the type of atmospheric system, and rainfall at the coast appears to be intensified by frictional processes. Estimates of evaporation minus precipitation are less negative than earlier ones; consideration of their relation to surface salinity leads to distributions that are in good agreement with oceanographic knowledge. The newer values suggest that in this region the heat gain by the atmosphere may be less (but moisture entrainment may be greater) than was thought. Close

• 33. [Article] A mesic maximum in biological water use demarcates biome sensitivity to aridity shifts

  Biome function is largely governed by how efficiently available resources can be used and yet for water, the ratio of direct biological resource use (transpiration, E_T) to total supply (annual precipitation, ...

  Citation × Citation Citation Abstract Copy Title: A mesic maximum in biological water use demarcates biome sensitivity to aridity shifts Author: Stephen P. Good Biome function is largely governed by how efficiently available resources can be used and yet for water, the ratio of direct biological resource use (transpiration, E_T) to total supply (annual precipitation, P) at ecosystem scales remains poorly characterized. Here, we synthesize field, remote sensing and ecohydrological modelling estimates to show that the biological water use fraction (E_T/P) reaches a maximum under mesic conditions; that is, when evaporative demand (potential evapotranspiration, E_P) slightly exceeds supplied precipitation. We estimate that this mesic maximum in E_T/P occurs at an aridity index (defined as E_P/P) between 1.3 and 1.9. The observed global average aridity of 1.8 falls within this range, suggesting that the biosphere is, on average, configured to transpire the largest possible fraction of global precipitation for the current climate. A unimodal E_T/P distribution indicates that both dry regions subjected to increasing aridity and humid regions subjected to decreasing aridity will suffer declines in the fraction of precipitation that plants transpire for growth and metabolism. Given the uncertainties in the prediction of future biogeography, this framework provides a clear and concise determination of ecosystems' sensitivity to climatic shifts, as well as expected patterns in the amount of precipitation that ecosystems can effectively use. Title: A mesic maximum in biological water use demarcates biome sensitivity to aridity shifts Author: Stephen P. Good Biome function is largely governed by how efficiently available resources can be used and yet for water, the ratio of direct biological resource use (transpiration, E_T) to total supply (annual precipitation, P) at ecosystem scales remains poorly characterized. Here, we synthesize field, remote sensing and ecohydrological modelling estimates to show that the biological water use fraction (E_T/P) reaches a maximum under mesic conditions; that is, when evaporative demand (potential evapotranspiration, E_P) slightly exceeds supplied precipitation. We estimate that this mesic maximum in E_T/P occurs at an aridity index (defined as E_P/P) between 1.3 and 1.9. The observed global average aridity of 1.8 falls within this range, suggesting that the biosphere is, on average, configured to transpire the largest possible fraction of global precipitation for the current climate. A unimodal E_T/P distribution indicates that both dry regions subjected to increasing aridity and humid regions subjected to decreasing aridity will suffer declines in the fraction of precipitation that plants transpire for growth and metabolism. Given the uncertainties in the prediction of future biogeography, this framework provides a clear and concise determination of ecosystems' sensitivity to climatic shifts, as well as expected patterns in the amount of precipitation that ecosystems can effectively use. Close

• 34. [Article] Trends in cation, nitrogen, sulfate and hydrogen ion concentrations in precipitation in the United States and Europe from 1978 to 2010: a new look at an old problem

  This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Springer and can be found at: http://link.springer.com/journal/10533.

  Citation × Citation Citation Abstract Copy Title: Trends in cation, nitrogen, sulfate and hydrogen ion concentrations in precipitation in the United States and Europe from 1978 to 2010: a new look at an old problem Author: Lajtha, Kate, Jones, Julia This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Springer and can be found at: http://link.springer.com/journal/10533. Title: Trends in cation, nitrogen, sulfate and hydrogen ion concentrations in precipitation in the United States and Europe from 1978 to 2010: a new look at an old problem Author: Lajtha, Kate, Jones, Julia This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Springer and can be found at: http://link.springer.com/journal/10533. Close

• 35. [Article] Assessing the Impact of Storm Regime on Remotely-sensed Precipitation Extremes Across the Western Himalaya

  Extreme, flood-producing precipitation events in mountains threaten human life and local and national economies. In the Himalayas, scarce meteorological data historically limited understanding of the underlying ...

  Citation × Citation Citation Abstract Copy Title: Assessing the Impact of Storm Regime on Remotely-sensed Precipitation Extremes Across the Western Himalaya Author: Stanton, Alan L. Extreme, flood-producing precipitation events in mountains threaten human life and local and national economies. In the Himalayas, scarce meteorological data historically limited understanding of the underlying processes driving extreme events. However, the capacity to observe, measure and quantify precipitation on regional scales has increased tremendously over the last three decades with the increasing prevalence of remotely-sensed data. While remotely-sensed precipitation can add essential information for understanding local hydrology, the spatial and temporal scales of the observations may result in biases based on the types of events that can be captured by the data. We analyze one of the recent remotely-sensed precipitation datasets, collected by the Tropical Rainfall Measuring Mission (TRMM), to better understand the spatial and temporal context of storm processes that generate flood disasters in high mountain environments. The objectives of this study are to 1) analyze the spatial distribution of extreme rainfall and convection across the mountain systems of the western Himalayan region, 2) investigate the deviations between remotely-sensed and ground-based precipitation observations across the orography, and 3) examine the sub-grid heterogeneity of remotely-sensed precipitation observations. First, we provide evidence of significant deviations between the mean and variance of extreme rainfall and convective intensities across mountain systems, which may produce variable over and underestimations of precipitation across the landscape. Extreme rainfall values are highest across the Lower Himalaya where synoptic weather systems are more prevalent, whereas extreme convective intensities are significantly higher across the Inner Himalaya. Second, we identify that deviations between extreme precipitation values measured by TRMM and GBO stations reverse with increasing topography, indicating that both rainfall regime and valley-ridge rainfall distributions vary with elevation and relief. Third, we identify large sub-grid differences in the variance of the extreme rainfall distributions within a single TRMM pixel, underscoring the complexities of bias correction of gridded rainfall measurements using GBO stations. Our findings support the hypothesis that storm regimes vary with the orography, uniquely affecting the measurement of remotely-sensed precipitation. Title: Assessing the Impact of Storm Regime on Remotely-sensed Precipitation Extremes Across the Western Himalaya Author: Stanton, Alan L. Extreme, flood-producing precipitation events in mountains threaten human life and local and national economies. In the Himalayas, scarce meteorological data historically limited understanding of the underlying processes driving extreme events. However, the capacity to observe, measure and quantify precipitation on regional scales has increased tremendously over the last three decades with the increasing prevalence of remotely-sensed data. While remotely-sensed precipitation can add essential information for understanding local hydrology, the spatial and temporal scales of the observations may result in biases based on the types of events that can be captured by the data. We analyze one of the recent remotely-sensed precipitation datasets, collected by the Tropical Rainfall Measuring Mission (TRMM), to better understand the spatial and temporal context of storm processes that generate flood disasters in high mountain environments. The objectives of this study are to 1) analyze the spatial distribution of extreme rainfall and convection across the mountain systems of the western Himalayan region, 2) investigate the deviations between remotely-sensed and ground-based precipitation observations across the orography, and 3) examine the sub-grid heterogeneity of remotely-sensed precipitation observations. First, we provide evidence of significant deviations between the mean and variance of extreme rainfall and convective intensities across mountain systems, which may produce variable over and underestimations of precipitation across the landscape. Extreme rainfall values are highest across the Lower Himalaya where synoptic weather systems are more prevalent, whereas extreme convective intensities are significantly higher across the Inner Himalaya. Second, we identify that deviations between extreme precipitation values measured by TRMM and GBO stations reverse with increasing topography, indicating that both rainfall regime and valley-ridge rainfall distributions vary with elevation and relief. Third, we identify large sub-grid differences in the variance of the extreme rainfall distributions within a single TRMM pixel, underscoring the complexities of bias correction of gridded rainfall measurements using GBO stations. Our findings support the hypothesis that storm regimes vary with the orography, uniquely affecting the measurement of remotely-sensed precipitation. Close

• 36. [Article] Buoy and satellite observation of wind induced surface heat exchange in the intraseasonal oscillation over West Pacific and Indian Ocean

  The importance of wind-driven latent heat fluxes for supporting tropical intraseasonal precipitation variability is analyzed. Tropical intraseasonal variability in the west pacific and Indian ocean is ...

  Citation × Citation Citation Abstract Copy Title: Buoy and satellite observation of wind induced surface heat exchange in the intraseasonal oscillation over West Pacific and Indian Ocean Author: Araligidad, Nilesh The importance of wind-driven latent heat fluxes for supporting tropical intraseasonal precipitation variability is analyzed. Tropical intraseasonal variability in the west pacific and Indian ocean is analyzed for northern and southern hemisphere summer during 1999-2005 using satellite and buoy observations. A composite analysis of QuikSCAT ocean vector winds and TRMM precipitation for the intraseasonal oscillation (ISO) indicate that enhanced precipitation is associated with anomalous surface westerly flow over the west Pacific and the Indian oceans. Anomalous westerly flow associated with the ISO is also accompanied by enhanced wind speed over the west Pacific and Indian ocean. Enhanced wind speed during westerly phases in the west Pacific and Indian oceans suggests an increase in the wind-driven component of latent heat flux. An analysis using TAO buoys and TRMM precipitation shows a significant correlation between intraseasonal (30-100 day) latent heat flux and TRMM precipitation in the region where enhanced precipitation occurs during the ISO westerly phase. Latent heat flux anomalies are about 20% of precipitation anomalies, a magnitude approximately sufficient as suggested by previous studies to support a flux-driven convective instability. The correlation of QuikSCAT wind speed and TRMM precipitation was analyzed over the west Pacific and it also showed a correlation of similar magnitude as the correlation of latent heat flux and precipitation. As a sensitivity test to determine how much of the latent heat flux anomalies were wind-driven, latent heat flux anomalies were recalculated at the location of strong correlation by fixing SST, boundary layer relative humidity, and boundary layer temperature to their sixty days running averages. This sensitivity analysis shows that most of the latent heat flux anomaly is wind-driven, indicating that intraseasonal precipitation may be supported by a wind-evaporation feedback mechanism. Wind speed and precipitation anomalies also show a significant correlation in the Indian ocean. This result suggests that if latent heat flux anomalies in the Indian ocean are primarily wind-driven, then a wind-evaporation feedback mechanism may also be supported there. Title: Buoy and satellite observation of wind induced surface heat exchange in the intraseasonal oscillation over West Pacific and Indian Ocean Author: Araligidad, Nilesh The importance of wind-driven latent heat fluxes for supporting tropical intraseasonal precipitation variability is analyzed. Tropical intraseasonal variability in the west pacific and Indian ocean is analyzed for northern and southern hemisphere summer during 1999-2005 using satellite and buoy observations. A composite analysis of QuikSCAT ocean vector winds and TRMM precipitation for the intraseasonal oscillation (ISO) indicate that enhanced precipitation is associated with anomalous surface westerly flow over the west Pacific and the Indian oceans. Anomalous westerly flow associated with the ISO is also accompanied by enhanced wind speed over the west Pacific and Indian ocean. Enhanced wind speed during westerly phases in the west Pacific and Indian oceans suggests an increase in the wind-driven component of latent heat flux. An analysis using TAO buoys and TRMM precipitation shows a significant correlation between intraseasonal (30-100 day) latent heat flux and TRMM precipitation in the region where enhanced precipitation occurs during the ISO westerly phase. Latent heat flux anomalies are about 20% of precipitation anomalies, a magnitude approximately sufficient as suggested by previous studies to support a flux-driven convective instability. The correlation of QuikSCAT wind speed and TRMM precipitation was analyzed over the west Pacific and it also showed a correlation of similar magnitude as the correlation of latent heat flux and precipitation. As a sensitivity test to determine how much of the latent heat flux anomalies were wind-driven, latent heat flux anomalies were recalculated at the location of strong correlation by fixing SST, boundary layer relative humidity, and boundary layer temperature to their sixty days running averages. This sensitivity analysis shows that most of the latent heat flux anomaly is wind-driven, indicating that intraseasonal precipitation may be supported by a wind-evaporation feedback mechanism. Wind speed and precipitation anomalies also show a significant correlation in the Indian ocean. This result suggests that if latent heat flux anomalies in the Indian ocean are primarily wind-driven, then a wind-evaporation feedback mechanism may also be supported there. Close

• 37. [Article] An Atmospheric Teleconnection Linking ENSO and Southwestern European Precipitation

  Numerous studies have demonstrated statistical associations between the El Niño–Southern Oscillation (ENSO) and precipitation in the Mediterranean basin. The dynamical bases for these teleconnections have ...

  Citation × Citation Citation Abstract Copy Title: An Atmospheric Teleconnection Linking ENSO and Southwestern European Precipitation Author: Tziperman, Eli, Shaman, Jeffrey Numerous studies have demonstrated statistical associations between the El Niño–Southern Oscillation (ENSO) and precipitation in the Mediterranean basin. The dynamical bases for these teleconnections have yet to be fully identified. Here, observational analyses and model simulations are used to show how ENSO variability affects rainfall over southwestern Europe (Iberia, Southern France, and Italy). A precipitation index for the region, named southwestern European Precipitation (SWEP), is used. The observational analyses show that ENSO modulates SWEP during the September–December wet season. These precipitation anomalies are associated with changes in large-scale atmospheric fields to the west of Iberia that alter low-level westerly winds and onshore moisture advection from the Atlantic. The vorticity anomalies associated with SWEP variability are linked to ENSO through a stationary barotropic Rossby wave train that emanates from the eastern equatorial Pacific and propagates eastward to the Atlantic and Mediterranean. Solutions of the linearized barotropic vorticity equation produce such eastward-propagating Rossby waves with trajectories that traverse the region of observed ENSO-related anomalies. In addition, these linearized barotropic vorticity equation solutions produce a dipole of positive and negative vorticity anomalies to the west of Iberia that matches observations and is consistent with the onshore advection of moisture. Thus, interannual variability of fall and early winter precipitation over southwestern Europe is linked to ENSO variability in the eastern Pacific via an eastward-propagating atmospheric stationary barotropic Rossby wave train. Title: An Atmospheric Teleconnection Linking ENSO and Southwestern European Precipitation Author: Tziperman, Eli, Shaman, Jeffrey Numerous studies have demonstrated statistical associations between the El Niño–Southern Oscillation (ENSO) and precipitation in the Mediterranean basin. The dynamical bases for these teleconnections have yet to be fully identified. Here, observational analyses and model simulations are used to show how ENSO variability affects rainfall over southwestern Europe (Iberia, Southern France, and Italy). A precipitation index for the region, named southwestern European Precipitation (SWEP), is used. The observational analyses show that ENSO modulates SWEP during the September–December wet season. These precipitation anomalies are associated with changes in large-scale atmospheric fields to the west of Iberia that alter low-level westerly winds and onshore moisture advection from the Atlantic. The vorticity anomalies associated with SWEP variability are linked to ENSO through a stationary barotropic Rossby wave train that emanates from the eastern equatorial Pacific and propagates eastward to the Atlantic and Mediterranean. Solutions of the linearized barotropic vorticity equation produce such eastward-propagating Rossby waves with trajectories that traverse the region of observed ENSO-related anomalies. In addition, these linearized barotropic vorticity equation solutions produce a dipole of positive and negative vorticity anomalies to the west of Iberia that matches observations and is consistent with the onshore advection of moisture. Thus, interannual variability of fall and early winter precipitation over southwestern Europe is linked to ENSO variability in the eastern Pacific via an eastward-propagating atmospheric stationary barotropic Rossby wave train. Close

• 38. [Article] Satellite and Buoy Observations of Boreal Summer Intraseasonal Variability in the Tropical Northeast Pacific

  Tropical intraseasonal variability in the eastern North Pacific during June–September of 2000–03 is analyzed using satellite and buoy observations. Quick Scatterometer ocean vector winds and the Tropical Rainfall ...

  Citation × Citation Citation Abstract Copy Title: Satellite and Buoy Observations of Boreal Summer Intraseasonal Variability in the Tropical Northeast Pacific Author: Esbensen, Steven K., Maloney, Eric D. Tropical intraseasonal variability in the eastern North Pacific during June–September of 2000–03 is analyzed using satellite and buoy observations. Quick Scatterometer ocean vector winds and the Tropical Rainfall Measuring Mission (TRMM) precipitation indicate that periods of anomalous surface westerly flow over the east Pacific warm pool during a summertime intraseasonal oscillation (ISO) life cycle are generally associated with an enhancement of convection to the east of 120°W. An exception is a narrow band of suppressed precipitation along 8°N that is associated with negative column-integrated precipitable water anomalies and anticyclonic vorticity anomalies. Periods of surface easterly anomalies are generally associated with suppressed convection to the east of 120°W. Summertime wind jets in the Gulfs of Tehuantepec and Papagayo exhibit heightened activity during periods of ISO easterly anomalies and suppressed convection. Strong variations in east Pacific warm pool wind speed occur in association with the summertime ISO. Anomalous ISO westerly flow is generally accompanied by enhanced wind speed to the east of 120°W, while anomalous easterly flow is associated with suppressed wind speed. Intraseasonal vector wind anomalies added to the climatological flow account for the bulk of the wind speed enhancement in the warm pool during the westerly phase, while the easterly phase shows strong contributions to the negative wind speed anomaly from both intraseasonal vector wind anomalies and suppressed synoptic-scale eddy activity. An analysis using Tropical Atmosphere Ocean buoys and TRMM precipitation suggests that wind–evaporation feedback is important for supporting summertime intraseasonal convection over the east Pacific warm pool. A statistically significant correlation of 0.6 between intraseasonal latent heat flux and precipitation occurs at the 12°N, 95°W buoy. Correlations between precipitation and latent heat flux at the 10°N, 95°W and 8°N, 95°W buoys are positive (0.4), but not statistically significant. Intraseasonal latent heat flux anomalies at all buoys are primarily wind induced. Consistent with the suppressed convection there during the ISO westerly phase, a negative but not statistically significant correlation ( 0.3) occurs between precipitation and latent heat flux at the 8°N, 110°W buoy. Title: Satellite and Buoy Observations of Boreal Summer Intraseasonal Variability in the Tropical Northeast Pacific Author: Esbensen, Steven K., Maloney, Eric D. Tropical intraseasonal variability in the eastern North Pacific during June–September of 2000–03 is analyzed using satellite and buoy observations. Quick Scatterometer ocean vector winds and the Tropical Rainfall Measuring Mission (TRMM) precipitation indicate that periods of anomalous surface westerly flow over the east Pacific warm pool during a summertime intraseasonal oscillation (ISO) life cycle are generally associated with an enhancement of convection to the east of 120°W. An exception is a narrow band of suppressed precipitation along 8°N that is associated with negative column-integrated precipitable water anomalies and anticyclonic vorticity anomalies. Periods of surface easterly anomalies are generally associated with suppressed convection to the east of 120°W. Summertime wind jets in the Gulfs of Tehuantepec and Papagayo exhibit heightened activity during periods of ISO easterly anomalies and suppressed convection. Strong variations in east Pacific warm pool wind speed occur in association with the summertime ISO. Anomalous ISO westerly flow is generally accompanied by enhanced wind speed to the east of 120°W, while anomalous easterly flow is associated with suppressed wind speed. Intraseasonal vector wind anomalies added to the climatological flow account for the bulk of the wind speed enhancement in the warm pool during the westerly phase, while the easterly phase shows strong contributions to the negative wind speed anomaly from both intraseasonal vector wind anomalies and suppressed synoptic-scale eddy activity. An analysis using Tropical Atmosphere Ocean buoys and TRMM precipitation suggests that wind–evaporation feedback is important for supporting summertime intraseasonal convection over the east Pacific warm pool. A statistically significant correlation of 0.6 between intraseasonal latent heat flux and precipitation occurs at the 12°N, 95°W buoy. Correlations between precipitation and latent heat flux at the 10°N, 95°W and 8°N, 95°W buoys are positive (0.4), but not statistically significant. Intraseasonal latent heat flux anomalies at all buoys are primarily wind induced. Consistent with the suppressed convection there during the ISO westerly phase, a negative but not statistically significant correlation ( 0.3) occurs between precipitation and latent heat flux at the 8°N, 110°W buoy. Close

• 39. [Article] Infrared thermography of evaporative fluxes and dynamics of salt deposition on heterogeneous porous surfaces

  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/wr/.

  Citation × Citation Citation Abstract Copy Title: Infrared thermography of evaporative fluxes and dynamics of salt deposition on heterogeneous porous surfaces Author: Shahraeeni, Ebrahim, Or, Dani, Weisbrod, Noam, Dragila, Maria, Nachshon, Uri 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/wr/. Title: Infrared thermography of evaporative fluxes and dynamics of salt deposition on heterogeneous porous surfaces Author: Shahraeeni, Ebrahim, Or, Dani, Weisbrod, Noam, Dragila, Maria, Nachshon, Uri 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/wr/. Close

• 40. [Article] Continuous precipitation of ceria nanoparticles from a continuous flow micromixer

  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: Continuous precipitation of ceria nanoparticles from a continuous flow micromixer Author: Tseng, Chih Heng T., Engelhard, Mark H., Chang, Chih-Hung, Paul, Brian K. 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://www.springer.com/?SGWID=0-102-0-0-0. Title: Continuous precipitation of ceria nanoparticles from a continuous flow micromixer Author: Tseng, Chih Heng T., Engelhard, Mark H., Chang, Chih-Hung, Paul, Brian K. 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://www.springer.com/?SGWID=0-102-0-0-0. Close