Micromet Methods for Determining Fluxes of Nitrogen Species. Tilden P. Meyers NOAA/ARL Atmospheric Turbulence and Diffusion Division Oak Ridge, TN

Size: px
Start display at page:

Download "Micromet Methods for Determining Fluxes of Nitrogen Species. Tilden P. Meyers NOAA/ARL Atmospheric Turbulence and Diffusion Division Oak Ridge, TN"

Transcription

1 Micromet Methods for Determining Fluxes of Nitrogen Species Tilden P. Meyers NOAA/ARL Atmospheric Turbulence and Diffusion Division Oak Ridge, TN

2 Presentation Objectives Discuss various methodologies to measure NH 3 exchange Highlight specific sampling considerations and guidelines for each method Present results from various field experiments

3 All micrometeorological methods are constrained by: 1. Fluxes don't vary in X,Y plane in the flux footprint 2. The exchange at the surface is same as that at sensor height

4 or NH 3, we often are interested in characterizing eposition as well as emission ission sources of NH 3 generally are aracterized by small areas that have atial scales less than a typical flux otprint (swine lagoons, poultry farms,.) position targets are vegetation asslands, forests, crops, soil) that can e considerable spatial extent, but are en located in areas that have small NH 3 centrations

5 For characterizing NH 3 emissions Integrated Mass Balance Average emission rate = what is advected past tower

6 Flux = z 0 u z c z dz ( ) ( ) r Similarly, inverse Lagrangian methods have been used to estimate the mean source area emission strength from measurements of NH3 concentrations downwind of the source area. (Flesch et al, 1995, J. Applied Meteorology) (Kljun, et al., 2002, Boundary-Layer Meteorology)

7 he application of micromet methods is not limited the micromet state of the art but by the current ethods used to measure the trace gas of interest H 3 ). st time response (> 1 Hz) eddy covariance ow but accurate gradient methods (AM,MBR) ccumulation methods (conditional sampling (REA)

8

9

10 Eddy covariance Eddy covariance is inherently a noise rejection method as the high number of samples in an averaging period (30 min 60 min) will average out if errors are random with a mean of 0. Useful results can be obtained even with low signal/noise ratios. Emission flux+ w+,c+, w-,c-, w ' c' + Deposition fluxw-,c+, w+,c-, w ' c' -

11 Good time resolution Advantages of Eddy Covariance Inherently a noise rejection method > many samples Considerations Usually requires major power for pumps, etc. Usually not all weather instrumentation If using sampling tubes, tubes, and inlet losses

12 radient (Modified Bowen Ratio Method) Measure the flux (eddy covariance) and vertical gradient of constituent (heat, water vapour, CO 2 ) over specified height. Compute effective transfer coefficient (flux/gradient) Measure vertical gradient of NH 3 over same height interval and apply computed transfer coefficient to obtain a measure of the flux?c F NH3 =H??

13 Water vapor and CO 2 gradients To remove bias error, use same analyzer for both heights, switching at 30 sec to 5 min intervals and allowing for representative sampling. T c =cycletime Relative error e= 6 ( T / t) 0.8 c For T c = 60 s, τ = 30 s,? = 10% t=turbulencetimescale

14

15

16 Advantages of MBR Good for slow response trace gas sensors Adequate time resolution (30 min -> hour) Considerations Bias tests on surrogate scalars Bias test on trace gas gradient systems Sampling tube and inlet losses

17 Conditional Sampling Relaxed Eddy Accumulation For sampling gases and aerosols in accumulation devices like annular denuders, filterpacks, etc. Flux = βσ w (C up - C dn ) = empirical coefficient, 0.6 = standard deviation vertical velocity = average concentration of updrafts, downdrafts w up, C dn

18 What constitutes an updraft, etc.? Separate w into three bins deadband +/ m/s dead accumulator updraft > 0.1 m/s up accumulator downdraft < -0.1 m/s down accumulator

19 Updraft Downdraft Deadband (mid)

20

21 Ammonia Fluxes (REA)? USDA/ARS-BARC J. Meisinger? NOAA/ARL W. Luke 20 l/min flow cyclone/impactor 2.5 µm cut-point citric acid (phosphoric) coated denuders 3-4 hour sample intervals

22 These plants could use a drink...mmh

23 Average Loss 1.5 kg N/ha/day

24 Advantages of REA When used with denuders and filterpacks, can sample several species at once (NH 3, NH 4, SO 2, SO 4, HNO 3, NO 3 ) Considerations Very manual intensive with denuders (cleaning, coating, exposing, extracting, IC analysis Sample flows and extraction volumes need to be measured very accurately

Measuring Carbon Using Micrometeorological Methods

Measuring Carbon Using Micrometeorological Methods Measuring Carbon Using Micrometeorological Methods Theory Theory Sink = Vertical Transport + Change in Horizontal Transport + Change in Storage + Diffusion Storage within walls Diffusion across walls Transport

More information

Measurement of Ammonia Concentrations and Fluxes: Recent Examples Using Denuder and Chemiluminescence Technologies

Measurement of Ammonia Concentrations and Fluxes: Recent Examples Using Denuder and Chemiluminescence Technologies Measurement of Ammonia Concentrations and Fluxes: Recent Examples Using Denuder and Chemiluminescence Technologies John Walker U.S. Environmental Protection Agency National Risk Management Research Laboratory

More information

EVALUATING LAND SURFACE FLUX OF METHANE AND NITROUS OXIDE IN AN AGRICULTURAL LANDSCAPE WITH TALL TOWER MEASUREMENTS AND A TRAJECTORY MODEL

EVALUATING LAND SURFACE FLUX OF METHANE AND NITROUS OXIDE IN AN AGRICULTURAL LANDSCAPE WITH TALL TOWER MEASUREMENTS AND A TRAJECTORY MODEL 8.3 EVALUATING LAND SURFACE FLUX OF METHANE AND NITROUS OXIDE IN AN AGRICULTURAL LANDSCAPE WITH TALL TOWER MEASUREMENTS AND A TRAJECTORY MODEL Xin Zhang*, Xuhui Lee Yale University, New Haven, CT, USA

More information

Fluxes: measurements and modeling. Flux

Fluxes: measurements and modeling. Flux Fluxes: measurements and modeling Schlesinger and Bernhardt Pg 135-150 Gustin flux paper Denmead, 2008 Baldocchi, 2012 Flux C time Amount of material transferred from one reservoir to the other Source

More information

in a Walnut Orchard During CHATS

in a Walnut Orchard During CHATS Aerosol Fluxes in a Walnut Orchard During CHATS Andreas Held 12 1,2, Alex Guenther 2, Ned Patton 2, Jim Smith 2, Andrew Turnipseed 2 1 Universität Bayreuth, Bayreuth, Germany 2 National Center for Atmospheric

More information

Techniques for measuring ammonia emissions from land applications of manure and fertiliser

Techniques for measuring ammonia emissions from land applications of manure and fertiliser NADP Ammonia Workshop, Washington DC, 22-24 October 2003 Techniques for measuring ammonia emissions from land applications of manure and fertiliser Tom Misselbrook and Fiona Nicholson Institute of Grassland

More information

Atmospheric and Depositional Nitrogen Monitoring J N Cape, Y S Tang, R I Smith, M A Sutton, E Nemitz, D Famulari, D Fowler

Atmospheric and Depositional Nitrogen Monitoring J N Cape, Y S Tang, R I Smith, M A Sutton, E Nemitz, D Famulari, D Fowler Atmospheric and Depositional Nitrogen Monitoring J N Cape, Y S Tang, R I Smith, M A Sutton, E Nemitz, D Famulari, D Fowler Centre for Ecology & Hydrology, Edinburgh, UK Sources of reactive N What to monitor

More information

This is the first of several lectures on flux measurements. We will start with the simplest and earliest method, flux gradient or K theory techniques

This is the first of several lectures on flux measurements. We will start with the simplest and earliest method, flux gradient or K theory techniques This is the first of several lectures on flux measurements. We will start with the simplest and earliest method, flux gradient or K theory techniques 1 Fluxes, or technically flux densities, are the number

More information

EVAPORATION GEOG 405. Tom Giambelluca

EVAPORATION GEOG 405. Tom Giambelluca EVAPORATION GEOG 405 Tom Giambelluca 1 Evaporation The change of phase of water from liquid to gas; the net vertical transport of water vapor from the surface to the atmosphere. 2 Definitions Evaporation:

More information

SRL TEE DRY DEPOSITION OF PARTICULATE MATTER ABOVE. Robert Lorenz and Charles E. Murphy, Jr.

SRL TEE DRY DEPOSITION OF PARTICULATE MATTER ABOVE. Robert Lorenz and Charles E. Murphy, Jr. TEE DRY DEPOSITION OF PARTICULATE MATTER ABOVE A LOBLOLLY PI~ PLARTATIOR - by Robert Lorenz and Charles E Murphy, Jr E I du Pent de Nemours & Company Savannah River Laboratory Aiken, South Carolina 29808

More information

Modelling atmospheric transport and deposition of ammonia and ammonium. Willem A.H. Asman Danish Institute of Agricultural Sciences

Modelling atmospheric transport and deposition of ammonia and ammonium. Willem A.H. Asman Danish Institute of Agricultural Sciences Modelling atmospheric transport and deposition of ammonia and ammonium Willem A.H. Asman Danish Institute of Agricultural Sciences Contents Processes Model results Conclusions Definitions NH 3 (ammonia)

More information

Footprints: outline Üllar Rannik University of Helsinki

Footprints: outline Üllar Rannik University of Helsinki Footprints: outline Üllar Rannik University of Helsinki -Concept of footprint and definitions -Analytical footprint models -Model by Korman and Meixner -Footprints for fluxes vs. concentrations -Footprints

More information

Surface-Atmosphere Exchange of Ammonia in a Non-fertilized Grassland and its Implications for PM 2.5

Surface-Atmosphere Exchange of Ammonia in a Non-fertilized Grassland and its Implications for PM 2.5 Surface-Atmosphere Exchange of Ammonia in a Non-fertilized Grassland and its Implications for PM 2.5 NADP 2013 Fall Meeting and Scientific Symposium October 10, 2013 Gregory R. Wentworth 1, P. Gregoire

More information

A new lidar for water vapor and temperature measurements in the Atmospheric Boundary Layer

A new lidar for water vapor and temperature measurements in the Atmospheric Boundary Layer A new lidar for water vapor and temperature measurements in the Atmospheric Boundary Layer M. Froidevaux 1, I. Serikov 2, S. Burgos 3, P. Ristori 1, V. Simeonov 1, H. Van den Bergh 1, and M.B. Parlange

More information

Deutscher Wetterdienst

Deutscher Wetterdienst Deutscher Wetterdienst Modelling the Volcanic Ash Episode: Experiences with COSMO-ART Detlev Majewski (FE1) Bernhard Vogel, Heike Vogel (KIT) Thomas Hanisch, Jochen Förstner (FE13), Ulrich Pflüger (FE15)

More information

Supplement of A dual-inlet, single detector relaxed eddy accumulation system for long-term measurement of mercury flux

Supplement of A dual-inlet, single detector relaxed eddy accumulation system for long-term measurement of mercury flux Supplement of Atmos. Meas. Tech., 9, 509 524, 2016 http://www.atmos-meas-tech.net/9/509/2016/ doi:10.5194/amt-9-509-2016-supplement Author(s) 2016. CC Attribution 3.0 License. Supplement of A dual-inlet,

More information

The Spatial Variability of Energy and Carbon Dioxide Fluxes at the Floor of a Deciduous Forest

The Spatial Variability of Energy and Carbon Dioxide Fluxes at the Floor of a Deciduous Forest University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. Bureau of Land Management Papers U.S. Department of the Interior 2001 The Spatial Variability of Energy and Carbon

More information

The Atmosphere. All of it. In one hour. Mikael Witte 10/27/2010

The Atmosphere. All of it. In one hour. Mikael Witte 10/27/2010 The Atmosphere All of it. In one hour. Mikael Witte 10/27/2010 Outline Structure Dynamics - heat transport Composition Trace constituent compounds Some Atmospheric Processes Ozone destruction in stratosphere

More information

Monoterpene and Sesquiterpene Emissions from Ponderosa Pine: Implications for Secondary Organic Aerosol Formation

Monoterpene and Sesquiterpene Emissions from Ponderosa Pine: Implications for Secondary Organic Aerosol Formation Monoterpene and Sesquiterpene Emissions from Ponderosa Pine: Implications for Secondary Organic Aerosol Formation Anita Lee, Gunnar Schade, Allen Goldstein UC Berkeley GCEP Workshop: August 19, 2002 What

More information

Validation of aerosols dry deposition velocity models with new experimental data

Validation of aerosols dry deposition velocity models with new experimental data Validation of aerosols dry deposition velocity models with new experimental data M. Talbaut 1, P.E. Damay 2, D. Maro 2, A. Coppalle 1, O. Connan 2, D. Hebert 2 1 UMR 6614 CORIA, St Etienne du Rouvray,

More information

Ammonia Emissions and Nitrogen Deposition in the United States and China

Ammonia Emissions and Nitrogen Deposition in the United States and China Ammonia Emissions and Nitrogen Deposition in the United States and China Presenter: Lin Zhang Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University Acknowledge: Daniel J.

More information

Measuring ammonia losses from pastures with micrometeorological methods

Measuring ammonia losses from pastures with micrometeorological methods Agroscope Measuring ammonia losses from pastures with micrometeorological methods Christof Ammann Federal Research Station Agroscope INH, Zürich, Switzerland with contributions from: Albrecht Neftel, Jörg

More information

EPS 236 Environmental Modeling and Analysis, Fall Term 2012

EPS 236 Environmental Modeling and Analysis, Fall Term 2012 EPS 236 Environmental Modeling and Analysis, Fall Term 2012 Prof. Steven C. Wofsy and Prof. Daniel J. Jacob Location: Geological Museum 105 (Daly Seminar Room) Time: Tuesday and Thursday, 6:00 to 7:30p

More information

Electromagnetic Radiation. Radiation and the Planetary Energy Balance. Electromagnetic Spectrum of the Sun

Electromagnetic Radiation. Radiation and the Planetary Energy Balance. Electromagnetic Spectrum of the Sun Radiation and the Planetary Energy Balance Electromagnetic Radiation Solar radiation warms the planet Conversion of solar energy at the surface Absorption and emission by the atmosphere The greenhouse

More information

Contents. 1. Evaporation

Contents. 1. Evaporation Contents 1 Evaporation 1 1a Evaporation from Wet Surfaces................... 1 1b Evaporation from Wet Surfaces in the absence of Advection... 4 1c Bowen Ratio Method........................ 4 1d Potential

More information

Wind Flow Modeling The Basis for Resource Assessment and Wind Power Forecasting

Wind Flow Modeling The Basis for Resource Assessment and Wind Power Forecasting Wind Flow Modeling The Basis for Resource Assessment and Wind Power Forecasting Detlev Heinemann ForWind Center for Wind Energy Research Energy Meteorology Unit, Oldenburg University Contents Model Physics

More information

Multiscale integral analysis of a HT leakage in a fusion nuclear power plant

Multiscale integral analysis of a HT leakage in a fusion nuclear power plant Journal of Physics: Conference Series PAPER OPEN ACCESS Multiscale integral analysis of a HT leakage in a fusion nuclear power plant To cite this article: M Velarde et al 2016 J. Phys.: Conf. Ser. 717

More information

The Importance of Ammonia in Modeling Atmospheric Transport and Deposition of Air Pollution. Organization of Talk:

The Importance of Ammonia in Modeling Atmospheric Transport and Deposition of Air Pollution. Organization of Talk: The Importance of Ammonia in Modeling Atmospheric Transport and Deposition of Air Pollution Organization of Talk: What is modeled Importance of NH 3 emissions to deposition Status of NH 3 emissions (model-based)

More information

Snow II: Snowmelt and energy balance

Snow II: Snowmelt and energy balance Snow II: Snowmelt and energy balance The are three basic snowmelt phases 1) Warming phase: Absorbed energy raises the average snowpack temperature to a point at which the snowpack is isothermal (no vertical

More information

Report from a construction site. Ulrich Dämmgen, Manfred Lüttich and Hans-Dieter Haenel

Report from a construction site. Ulrich Dämmgen, Manfred Lüttich and Hans-Dieter Haenel Emissions. atmospheric concentrations and bulk deposition of reduced nitrogen in Hesse. Germany steps towards a comprehensive treatment of reactive nitrogen in the atmosphere Report from a construction

More information

A GROUND-BASED PROCEDURE FOR ESTIMATING LATENT HEAT ENERGY FLUXES 1 Eric Harmsen 2, Richard Díaz 3 and Javier Chaparro 3

A GROUND-BASED PROCEDURE FOR ESTIMATING LATENT HEAT ENERGY FLUXES 1 Eric Harmsen 2, Richard Díaz 3 and Javier Chaparro 3 A GROUND-BASED PROCEDURE FOR ESTIMATING LATENT HEAT ENERGY FLUXES 1 Eric Harmsen 2, Richard Díaz 3 and Javier Chaparro 3 1. This material is based on research supported by NOAA-CREST and NASA-EPSCoR (NCC5-595).

More information

HT TRANSIENT THERMAL MEASUREMENTS USING THERMOGRAPHIC PHOSPHORS FOR TEMPERATURE RATE ESTIMATES

HT TRANSIENT THERMAL MEASUREMENTS USING THERMOGRAPHIC PHOSPHORS FOR TEMPERATURE RATE ESTIMATES Proceedings of HT2005 2005 ASME Summer Heat Transfer Conference July 17-22, 2005, San Francisco, California, USA HT2005-72464 TRANSIENT THERMAL MEASUREMENTS USING THERMOGRAPHIC PHOSPHORS FOR TEMPERATURE

More information

A Global Atmospheric Model. Joe Tribbia NCAR Turbulence Summer School July 2008

A Global Atmospheric Model. Joe Tribbia NCAR Turbulence Summer School July 2008 A Global Atmospheric Model Joe Tribbia NCAR Turbulence Summer School July 2008 Outline Broad overview of what is in a global climate/weather model of the atmosphere Spectral dynamical core Some results-climate

More information

Implementation of modules for wet and dry deposition into the ECMWF Integrated Forecast System

Implementation of modules for wet and dry deposition into the ECMWF Integrated Forecast System Implementation of modules for wet and dry deposition into the ECMWF Integrated Forecast System Johannes Flemming (ECMWF), Vincent Huijnen (KNMI) and Luke Jones (ECMWF) Deliverable D G-RG 4.6 1 Abstract

More information

MODELING THE FORMATION AND DEPOSITION OF ACIDIC POLLUTANTS

MODELING THE FORMATION AND DEPOSITION OF ACIDIC POLLUTANTS Atmospheric Deposition (Proceedings of the Baltimore Symposium, May 1989). IAHS Pub], No. 179. MODELING THE FORMATION AND DEPOSITION OF ACIDIC POLLUTANTS Chris J. Walcek Atmospheric Sciences Research Center,

More information

Evapotranspiration: Theory and Applications

Evapotranspiration: Theory and Applications Evapotranspiration: Theory and Applications Lu Zhang ( 张橹 ) CSIRO Land and Water Evaporation: part of our everyday life Evapotranspiration Global Land: P = 800 mm Q = 315 mm E = 485 mm Evapotranspiration

More information

Wind and turbulence experience strong gradients in vegetation. How do we deal with this? We have to predict wind and turbulence profiles through the

Wind and turbulence experience strong gradients in vegetation. How do we deal with this? We have to predict wind and turbulence profiles through the 1 2 Wind and turbulence experience strong gradients in vegetation. How do we deal with this? We have to predict wind and turbulence profiles through the canopy. 3 Next we discuss turbulence in the canopy.

More information

COST action OPTIMISE footprint modelling expert workshop

COST action OPTIMISE footprint modelling expert workshop COST action OPTIMISE footprint modelling expert workshop Place: University of Innsbruck Dates: 13-17.02.2017 Participants: Natascha Kljun (Swansea Univ., UK), Enrico Tomelleri (EURAC, Italy), Georg Wohlfahrt

More information

Disturbed micrometeorological flows example local advection

Disturbed micrometeorological flows example local advection Disturbed micrometeorological flows example local advection Horizontal gradients of mean properties ( u, T, u ' w ', w ' T ' etc.) in the atmospheric surface layer may be generated by inhomogeneity in

More information

Multi-Scale Modeling of Turbulence and Microphysics in Clouds. Steven K. Krueger University of Utah

Multi-Scale Modeling of Turbulence and Microphysics in Clouds. Steven K. Krueger University of Utah Multi-Scale Modeling of Turbulence and Microphysics in Clouds Steven K. Krueger University of Utah 10,000 km Scales of Atmospheric Motion 1000 km 100 km 10 km 1 km 100 m 10 m 1 m 100 mm 10 mm 1 mm Planetary

More information

Mercury Stack Monitor SM-4

Mercury Stack Monitor SM-4 Member of the envea Group Mercury Stack Monitor SM-4 Automatic continuous emission monitor (CEM) for mercury Continuous operation Sample dilution directly at stack - works with virtually any sample matrix

More information

Environmental Fluid Dynamics

Environmental Fluid Dynamics Environmental Fluid Dynamics ME EN 7710 Spring 2015 Instructor: E.R. Pardyjak University of Utah Department of Mechanical Engineering Definitions Environmental Fluid Mechanics principles that govern transport,

More information

Continuous measurement of airborne particles and gases

Continuous measurement of airborne particles and gases Continuous measurement of airborne particles and gases Jeff Collett and Taehyoung Lee Atmospheric Science Department Colorado State University Funding: USDA/AES and NPS Outline Why measure particles and

More information

Convective Mass Transfer

Convective Mass Transfer Convective Mass Transfer Definition of convective mass transfer: The transport of material between a boundary surface and a moving fluid or between two immiscible moving fluids separated by a mobile interface

More information

Spatial variations of CH 4 in surface air over Lake Taihu. Zhang Mi, Wang Shumin, Xu Jingzheng, Hu Cheng, Xiao Qitao

Spatial variations of CH 4 in surface air over Lake Taihu. Zhang Mi, Wang Shumin, Xu Jingzheng, Hu Cheng, Xiao Qitao Spatial variations of CH 4 in surface air over Lake Taihu Zhang Mi, Wang Shumin, Xu Jingzheng, Hu Cheng, Xiao Qitao 2014. 07. 18 Outline Introduction Objective Measurements Results Work plan 1. Introduction

More information

Supplement of Upside-down fluxes Down Under: CO 2 net sink in winter and net source in summer in a temperate evergreen broadleaf forest

Supplement of Upside-down fluxes Down Under: CO 2 net sink in winter and net source in summer in a temperate evergreen broadleaf forest Supplement of Biogeosciences, 15, 3703 3716, 2018 https://doi.org/10.5194/bg-15-3703-2018-supplement Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement

More information

Heat and Mass Transfer Unit-1 Conduction

Heat and Mass Transfer Unit-1 Conduction 1. State Fourier s Law of conduction. Heat and Mass Transfer Unit-1 Conduction Part-A The rate of heat conduction is proportional to the area measured normal to the direction of heat flow and to the temperature

More information

Introduction to Acid Deposition Monitoring (2) Dry Deposition Monitoring

Introduction to Acid Deposition Monitoring (2) Dry Deposition Monitoring Introduction to Acid Deposition Monitoring (2) Dry Deposition Monitoring ADORC Concept of dry deposition monitoring for EANET Dry Deposition Monitoring Air Concentration Monitoring Deposition Monitoring

More information

Incorporation of 3D Shortwave Radiative Effects within the Weather Research and Forecasting Model

Incorporation of 3D Shortwave Radiative Effects within the Weather Research and Forecasting Model Incorporation of 3D Shortwave Radiative Effects within the Weather Research and Forecasting Model W. O Hirok and P. Ricchiazzi Institute for Computational Earth System Science University of California

More information

Torben Königk Rossby Centre/ SMHI

Torben Königk Rossby Centre/ SMHI Fundamentals of Climate Modelling Torben Königk Rossby Centre/ SMHI Outline Introduction Why do we need models? Basic processes Radiation Atmospheric/Oceanic circulation Model basics Resolution Parameterizations

More information

Lecture 10 March 15, 2010, Monday. Atmospheric Pressure & Wind: Part 1

Lecture 10 March 15, 2010, Monday. Atmospheric Pressure & Wind: Part 1 Lecture 10 March 15, 2010, Monday Atmospheric Pressure & Wind: Part 1 Speed, Velocity, Acceleration, Force, Pressure Atmospheric Pressure & Its Measurement Ideal Gas Law (Equation of State) Pressure Gradient

More information

A THREE-DIMENSIONAL BACKWARD LAGRANGIAN FOOTPRINT MODEL FOR A WIDE RANGE OF BOUNDARY-LAYER STRATIFICATIONS. 1. Introduction

A THREE-DIMENSIONAL BACKWARD LAGRANGIAN FOOTPRINT MODEL FOR A WIDE RANGE OF BOUNDARY-LAYER STRATIFICATIONS. 1. Introduction A THREE-DIMENSIONAL BACKWARD LAGRANGIAN FOOTPRINT MODEL FOR A WIDE RANGE OF BOUNDARY-LAYER STRATIFICATIONS N. KLJUN 1,, M.W.ROTACH 1 and H. P. SCHMID 2 1 Institute for Atmospheric and Climate Science ETH,

More information

Coordinate rotation. Bernard Heinesch. Summer school : «eddy covariance flux measurements» Namur July 10th 20th, 2006

Coordinate rotation. Bernard Heinesch. Summer school : «eddy covariance flux measurements» Namur July 10th 20th, 2006 1 Coordinate rotation Bernard Heinesch 2 Outline Need for rotations Mathematical tools for coordinate rotation Angle determination Rotated every-period Classical 2D rotation 3rd rotation Long-term Planar

More information

A model for scalar advection inside canopies and application to footprint investigation

A model for scalar advection inside canopies and application to footprint investigation Agricultural and Forest Meteorology 127 (24) 131 141 www.elsevier.com/locate/agrformet A model for scalar advection inside canopies and application to footprint investigation Xuhui Lee School of Forestry

More information

2.1 OBSERVATIONS AND THE PARAMETERISATION OF AIR-SEA FLUXES DURING DIAMET

2.1 OBSERVATIONS AND THE PARAMETERISATION OF AIR-SEA FLUXES DURING DIAMET 2.1 OBSERVATIONS AND THE PARAMETERISATION OF AIR-SEA FLUXES DURING DIAMET Peter A. Cook * and Ian A. Renfrew School of Environmental Sciences, University of East Anglia, Norwich, UK 1. INTRODUCTION 1.1

More information

Exploration of Nitrogen Total Deposition Budget Uncertainty at the Regional Scale

Exploration of Nitrogen Total Deposition Budget Uncertainty at the Regional Scale Exploration of Nitrogen Total Deposition Budget Uncertainty at the Regional Scale Robin L. Dennis, Donna Schwede, Jesse Bash and Jon Pleim Atmospheric Modeling and Analysis Division NERL, EPA NADP Annual

More information

Atmospheric Mercury Deposition Modeling

Atmospheric Mercury Deposition Modeling Atmospheric Mercury Deposition Modeling Brief review and comments on remaining uncertainties Frank J. Marsik University of Michigan NADP Total Deposition Science Meeting October 28 th, 2011 Gaseous Dry

More information

The effect of turbulence and gust on sand erosion and dust entrainment during sand storm Xue-Ling Cheng, Fei Hu and Qing-Cun Zeng

The effect of turbulence and gust on sand erosion and dust entrainment during sand storm Xue-Ling Cheng, Fei Hu and Qing-Cun Zeng The effect of turbulence and gust on sand erosion and dust entrainment during sand storm Xue-Ling Cheng, Fei Hu and Qing-Cun Zeng State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric

More information

) was measured using net radiometers. Soil heat flux (Q g

) was measured using net radiometers. Soil heat flux (Q g Paper 4 of 18 Determination of Surface Fluxes Using a Bowen Ratio System V. C. K. Kakane* and E. K. Agyei Physics Department, University of Ghana, Legon, Ghana * Corresponding author, Email: vckakane@ug.edu.gh

More information

The Canadian ADAGIO Project for Mapping Total Atmospheric Deposition

The Canadian ADAGIO Project for Mapping Total Atmospheric Deposition The Canadian ADAGIO Project for Mapping Total Atmospheric Deposition Amanda S. Cole Environment & Climate Change Canada (ECCC) MMF-GTAD Workshop Geneva, Switzerland February 28, 2017 ADAGIO team Amanda

More information

The Challenge of. Guy Brasseur

The Challenge of. Guy Brasseur The Challenge of Monitoring and Predicting Chemical Weather Guy Brasseur Introduction: What is Chemical Weather? What is Chemical Weather? Local, regional, and global distributions of important trace gases

More information

Micro Chemical Vapor Deposition System: Design and Verification

Micro Chemical Vapor Deposition System: Design and Verification Micro Chemical Vapor Deposition System: Design and Verification Q. Zhou and L. Lin Berkeley Sensor and Actuator Center, Department of Mechanical Engineering, University of California, Berkeley 2009 IEEE

More information

Estimation of evapotranspiration using satellite TOA radiances Jian Peng

Estimation of evapotranspiration using satellite TOA radiances Jian Peng Estimation of evapotranspiration using satellite TOA radiances Jian Peng Max Planck Institute for Meteorology Hamburg, Germany Satellite top of atmosphere radiances Slide: 2 / 31 Surface temperature/vegetation

More information

Modeling of cloud microphysics: from simple concepts to sophisticated parameterizations. Part I: warm-rain microphysics

Modeling of cloud microphysics: from simple concepts to sophisticated parameterizations. Part I: warm-rain microphysics Modeling of cloud microphysics: from simple concepts to sophisticated parameterizations. Part I: warm-rain microphysics Wojciech Grabowski National Center for Atmospheric Research, Boulder, Colorado parameterization

More information

Convective Fluxes: Sensible and Latent Heat Convective Fluxes Convective fluxes require Vertical gradient of temperature / water AND Turbulence ( mixing ) Vertical gradient, but no turbulence: only very

More information

CHAPTER 1. MEASURES OF ATMOSPHERIC COMPOSITION

CHAPTER 1. MEASURES OF ATMOSPHERIC COMPOSITION 1 CHAPTER 1. MEASURES OF ATMOSPHERIC COMPOSITION The objective of atmospheric chemistry is to understand the factors that control the concentrations of chemical species in the atmosphere. In this book

More information

AIRCRAFT MEASUREMENTS OF ROUGHNESS LENGTHS FOR SENSIBLE AND LATENT HEAT OVER BROKEN SEA ICE

AIRCRAFT MEASUREMENTS OF ROUGHNESS LENGTHS FOR SENSIBLE AND LATENT HEAT OVER BROKEN SEA ICE Ice in the Environment: Proceedings of the 16th IAHR International Symposium on Ice Dunedin, New Zealand, 2nd 6th December 2002 International Association of Hydraulic Engineering and Research AIRCRAFT

More information

of Nebraska - Lincoln

of Nebraska - Lincoln University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Civil Engineering Faculty Publications Civil Engineering 2014 On the Equality Assumption of Latent and Sensible Heat Energy

More information

Emission of pesticides into the air

Emission of pesticides into the air during and after application to a potato crop F. van den Berg 1, H.J. Holterman 2 and M. Leistra 1 1 Alterra, Centre for Water and Climate 2 Plant Research International Contents Introduction Description

More information

Lecture 3. The Kinetic Molecular Theory of Gases

Lecture 3. The Kinetic Molecular Theory of Gases Lecture 3. The Kinetic Molecular Theory of Gases THE IDEAL GAS LAW: A purely empirical law solely the consequence of experimental observations Explains the behavior of gases over a limited range of conditions

More information

Eric Mougin & Josiane Seghieri CESBIO. TT members : 20 european teams 6 malian institutions

Eric Mougin & Josiane Seghieri CESBIO. TT members : 20 european teams 6 malian institutions TT3 EOP integrative studies on the Gourma meso-scale site (Mali) Eric Mougin & Josiane Seghieri CESBIO TT members : 20 european teams 6 malian institutions The AMMA meso-scale sites Gourma Niamey Ouémé

More information

The role of sea ice algae in Arctic marine ecosystems and oceanic emissions of dimethylsulfide. Hakase Hayashida Candidacy Exam August 19, 2015

The role of sea ice algae in Arctic marine ecosystems and oceanic emissions of dimethylsulfide. Hakase Hayashida Candidacy Exam August 19, 2015 The role of sea ice algae in Arctic marine ecosystems and oceanic emissions of dimethylsulfide Hakase Hayashida Candidacy Exam August 19, 2015 Introduction: Role of sea ice algae in Arctic marine ecosystems

More information

Measuring Total Reactive N and its Composition

Measuring Total Reactive N and its Composition Measuring Total Reactive N and its Composition Bret A. Schichtel 1, Katie Benedict 2, Christian M. Carrico 2, Anthony Prenni 2, Jr. 2, Ezra Levin 2, Derek Day 3, Doris Chen 2, John Ray 1, William C. Malm

More information

GAW - WCCAP recommendation for aerosol inlets and sampling tubes

GAW - WCCAP recommendation for aerosol inlets and sampling tubes GAW - WCCAP recommendation for aerosol inlets and sampling tubes Alfred Wiedensohler, Wolfram Birmili, Leibniz Institute for Tropospheric Research, Leipzig, Germany John Ogren, NOAA ESRL GMD, Boulder,

More information

What is PRECIS? The Physical Parameters Boundary Conditions Why the Mediterranean Basin? The Sulfur Cycle & Aerosols Aerosols Impacts Data Analysis

What is PRECIS? The Physical Parameters Boundary Conditions Why the Mediterranean Basin? The Sulfur Cycle & Aerosols Aerosols Impacts Data Analysis What is PRECIS? The Physical Parameters Boundary Conditions Why the Mediterranean Basin? The Sulfur Cycle & Aerosols Aerosols Impacts Data Analysis Sulfur Cycle Validation Future Scenarios Conclusions

More information

Part I: Dry Convection

Part I: Dry Convection Turbulent dispersion and chemical transformation in the atmospheric boundary layer: Part I: Dry Convection DISPERSION Thanks: Alessandro Dosio Jordi Vilà-Guerau de Arellano WA G E N I N G E N U N I VE

More information

Guidelines on Quality Control Procedures for Data from Automatic Weather Stations

Guidelines on Quality Control Procedures for Data from Automatic Weather Stations Guidelines on Quality Control Procedures for Data from Automatic Weather Stations Igor Zahumenský Slovak Hydrometeorological Institute SHMI, Jeséniova 17, 833 15 Bratislava, Slovakia Tel./Fax. +421 46

More information

MATHEMATICAL MODEL OF A VAPOUR ABSORPTION REFRIGERATION UNIT

MATHEMATICAL MODEL OF A VAPOUR ABSORPTION REFRIGERATION UNIT ISSN 1726-4529 Int j simul model 9 (2010) 2, 86-97 Original scientific paper MATHEMATICAL MODEL OF A VAPOUR ABSORPTION REFRIGERATION UNIT Micallef, D. & Micallef, C. University of Malta, Department of

More information

Aerosols AP sizes AP types Sources Sinks Amount and lifetime Aerosol radiative effects. Aerosols. Trude Storelvmo Aerosols 1 / 21

Aerosols AP sizes AP types Sources Sinks Amount and lifetime Aerosol radiative effects. Aerosols. Trude Storelvmo Aerosols 1 / 21 Aerosols Trude Storelvmo Aerosols 1 / 21 Aerosols: Definition Definition of an aerosol: disperse system with air as carrier gas and a solid or liquid or a mixture of both as disperse phases. Aerosol particles

More information

Gas transfer rates If either phase concentration can not be predicted by Henry's law then there will be a transfer of mass across the interface until

Gas transfer rates If either phase concentration can not be predicted by Henry's law then there will be a transfer of mass across the interface until Gas transfer rates If either phase concentration can not be predicted by Henry's law then there will be a transfer of mass across the interface until equilibrium is reached. The mechanisms and rate expressions

More information

Land Surface Processes and Their Impact in Weather Forecasting

Land Surface Processes and Their Impact in Weather Forecasting Land Surface Processes and Their Impact in Weather Forecasting Andrea Hahmann NCAR/RAL with thanks to P. Dirmeyer (COLA) and R. Koster (NASA/GSFC) Forecasters Conference Summer 2005 Andrea Hahmann ATEC

More information

Standard Practices for Air Speed Calibration Testing

Standard Practices for Air Speed Calibration Testing Standard Practices for Air Speed Calibration Testing Rachael V. Coquilla Bryza Wind Lab, Fairfield, California Air speed calibration is a test process where the output from a wind measuring instrument

More information

1. Composition and Structure

1. Composition and Structure Atmospheric sciences focuses on understanding the atmosphere of the earth and other planets. The motivations for studying atmospheric sciences are largely: weather forecasting, climate studies, atmospheric

More information

Some remarks on climate modeling

Some remarks on climate modeling Some remarks on climate modeling A. Gettelman & J. J. Hack National Center for Atmospheric Research Boulder, Colorado USA Selected overheads by Doug Nychka Outline Hierarchy of atmospheric modeling strategies

More information

Comparing independent estimates of carbon dioxide exchange over 5 years at a deciduous forest in the southeastern United States

Comparing independent estimates of carbon dioxide exchange over 5 years at a deciduous forest in the southeastern United States JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. D24, PAGES 34,167 34,178, DECEMBER 27, 2001 Comparing independent estimates of carbon dioxide exchange over 5 years at a deciduous forest in the southeastern

More information

Effect of Turbulent Enhancemnt of Collision-coalescence on Warm Rain Formation in Maritime Shallow Convection

Effect of Turbulent Enhancemnt of Collision-coalescence on Warm Rain Formation in Maritime Shallow Convection Effect of Turbulent Enhancemnt of Collision-coalescence on Warm Rain Formation in Maritime Shallow Convection A. A. WYSZOGRODZKI 1 W. W. GRABOWSKI 1,, L.-P. WANG 2, AND O. AYALA 2 1 NATIONAL CENTER FOR

More information

Remote sensing estimates of actual evapotranspiration in an irrigation district

Remote sensing estimates of actual evapotranspiration in an irrigation district Engineers Australia 29th Hydrology and Water Resources Symposium 21 23 February 2005, Canberra Remote sensing estimates of actual evapotranspiration in an irrigation district Cressida L. Department of

More information

Chapter 3- Energy Balance and Temperature

Chapter 3- Energy Balance and Temperature Chapter 3- Energy Balance and Temperature Understanding Weather and Climate Aguado and Burt Influences on Insolation Absorption Reflection/Scattering Transmission 1 Absorption An absorber gains energy

More information

Surface Energy Budget

Surface Energy Budget Surface Energy Budget Please read Bonan Chapter 13 Energy Budget Concept For any system, (Energy in) (Energy out) = (Change in energy) For the land surface, Energy in =? Energy Out =? Change in energy

More information

Faculty of Environmental Sciences, Department of Hydrosciences, Chair of Meteorology

Faculty of Environmental Sciences, Department of Hydrosciences, Chair of Meteorology Faculty of Environmental Sciences, Department of Hydrosciences, Chair of Meteorology Effects of Measurement Uncertainties of Meteorological Data on Estimates of Site Water Balance Components PICO presentation

More information

Note the diverse scales of eddy motion and self-similar appearance at different lengthscales of the turbulence in this water jet. Only eddies of size

Note the diverse scales of eddy motion and self-similar appearance at different lengthscales of the turbulence in this water jet. Only eddies of size L Note the diverse scales of eddy motion and self-similar appearance at different lengthscales of the turbulence in this water jet. Only eddies of size 0.01L or smaller are subject to substantial viscous

More information

Lecture notes: Interception and evapotranspiration

Lecture notes: Interception and evapotranspiration Lecture notes: Interception and evapotranspiration I. Vegetation canopy interception (I c ): Portion of incident precipitation (P) physically intercepted, stored and ultimately evaporated from vegetation

More information

The Art and Role of Climate Modeling

The Art and Role of Climate Modeling Institute of Coastal Research, GKSS Research Centre Geesthacht, Hans von Storch The Art and Role of Climate Modeling Overview: 1. Conceptual aspects of modelling 2. Conceptual models for the reduction

More information

Regional methane emissions estimates in northern Pennsylvania gas fields using a mesoscale atmospheric inversion system

Regional methane emissions estimates in northern Pennsylvania gas fields using a mesoscale atmospheric inversion system Regional methane emissions estimates in northern Pennsylvania gas fields using a mesoscale atmospheric inversion system Thomas Lauvaux1, A. Deng1, B. Gaudet1, S. J. Richardson1, N. L. Miles1, J. N. Ciccarelli1,2,

More information

ATMO. Theoretical considerations on the energy balance closure. Frederik De Roo and Matthias Mauder

ATMO. Theoretical considerations on the energy balance closure. Frederik De Roo and Matthias Mauder ATMO Theoretical considerations on the energy balance closure Frederik De Roo and Matthias Mauder Karlsruhe Institute of Technology, Campus Alpin Atmospheric Environmental Research (KIT/IMK-IFU) Garmisch-Partenkirchen

More information

One-Dimensional Models

One-Dimensional Models One-Dimensional Models GCC Summer School, 2005 Banff, Alberta Dylan Jones Department of Physics University of Toronto Observations and Models Observations Models Envelope of M-O variance Criteria for model

More information

Investigation of the Air-Wave-Sea Interaction Modes Using an Airborne Doppler Wind Lidar: Analyses of the HRDL data taken during DYNAMO

Investigation of the Air-Wave-Sea Interaction Modes Using an Airborne Doppler Wind Lidar: Analyses of the HRDL data taken during DYNAMO DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Investigation of the Air-Wave-Sea Interaction Modes Using an Airborne Doppler Wind Lidar: Analyses of the HRDL data taken

More information

Review of Anemometer Calibration Standards

Review of Anemometer Calibration Standards Review of Anemometer Calibration Standards Rachael V. Coquilla rvcoquilla@otechwind.com Otech Engineering, Inc., Davis, CA Anemometer calibration defines a relationship between the measured signals from

More information

Daniel J. Jacob, Models of Atmospheric Transport and Chemistry, 2007.

Daniel J. Jacob, Models of Atmospheric Transport and Chemistry, 2007. 1 0. CHEMICAL TRACER MODELS: AN INTRODUCTION Concentrations of chemicals in the atmosphere are affected by four general types of processes: transport, chemistry, emissions, and deposition. 3-D numerical

More information

Supporting Information for. Measuring Emissions from Oil and Natural Gas. Well Pads Using the Mobile Flux Plane Technique

Supporting Information for. Measuring Emissions from Oil and Natural Gas. Well Pads Using the Mobile Flux Plane Technique Supporting Information for Measuring Emissions from Oil and Natural Gas Well Pads Using the Mobile Flux Plane Technique Chris W. Rella*, Tracy R. Tsai, Connor G. Botkin, Eric R. Crosson, David Steele This

More information