The LAGRANTO Lagrangian analysis tool – version 2.0

Abstract. Lagrangian trajectories are widely used in the atmospheric sciences, for instance to identify flow structures in extratropical cyclones (e.g., warm conveyor belts) and long-range transport pathways of moisture and trace substances. Here a new version of the Lagrangian analysis tool LAGRANTO (Wernli and Davies, 1997) is introduced, which offers considerably enhanced functionalities. Trajectory starting positions can be defined easily and flexibly based on different geometrical and/or meteorological conditions, e.g., equidistantly spaced within a prescribed region and on a stack of pressure (or isentropic) levels. After the computation of the trajectories, a versatile selection of trajectories is offered based on single or combined criteria. These criteria are passed to LAGRANTO with a simple command language (e.g., "GT:PV:2" readily translates into a selection of all trajectories with potential vorticity, PV, greater than 2 PVU; 1 PVU = 10−6 K m2 kg−1 s−1). Full versions of this new version of LAGRANTO are available for global ECMWF and regional COSMO data, and core functionality is provided for the regional WRF and MetUM models and the global 20th Century Reanalysis data set. The paper first presents the intuitive application of LAGRANTO for the identification of a warm conveyor belt in the North Atlantic. A further case study then shows how LAGRANTO can be used to quasi-operationally diagnose stratosphere–troposphere exchange events. Whereas these examples rely on the ECMWF version, the COSMO version and input fields with 7 km horizontal resolution serve to resolve the rather complex flow structure associated with orographic blocking due to the Alps, as shown in a third example. A final example illustrates the tool's application in source–receptor analysis studies. The new distribution of LAGRANTO is publicly available and includes auxiliary tools, e.g., to visualize trajectories. A detailed user guide describes all LAGRANTO capabilities.

[1]  Holger Vömel,et al.  Particle backscatter and relative humidity measured across cirrus clouds and comparison with microphysical cirrus modelling , 2012 .

[2]  Heini Wernli,et al.  Influence of microphysical processes on the potential vorticity development in a warm conveyor belt: a case‐study with the limited‐area model COSMO , 2012 .

[3]  H. Wernli,et al.  A Lagrangian Climatology of Tropical Moisture Exports to the Northern Hemispheric Extratropics , 2009 .

[4]  M. Bevis,et al.  Locating a point on a spherical surface relative to a spherical polygon of arbitrary shape , 1989 .

[5]  J. D. Price,et al.  Transport into the troposphere in a tropopause fold , 1994 .

[6]  Heini Wernli,et al.  A Lagrangian‐based analysis of extratropical cyclones. I: The method and some applications , 1997 .

[7]  Heini Wernli,et al.  Warm Conveyor Belts in the ERA-Interim Dataset (1979–2010). Part II: Moisture Origin and Relevance for Precipitation , 2014 .

[8]  Natascha Kljun,et al.  Frontal modification and lee cyclogenesis in the Alps: A case study using the ALPEX reanalysis data set , 2001 .

[9]  Michael Garstang,et al.  Saharan dust in the Amazon Basin , 1992 .

[10]  Petra Seibert Convergence and Accuracy of Numerical Methods for Trajectory Calculations , 1993 .

[11]  Harald Sodemann,et al.  Planning aircraft measurements within a warm conveyor belt , 2014 .

[12]  Heini Wernli,et al.  Air parcel trajectory analysis of stable isotopes in water vapor in the eastern Mediterranean , 2008 .

[13]  Mark R. Schoeberl,et al.  A reinterpretation of the data from the NASA Stratosphere‐Troposphere Exchange Project , 1995 .

[14]  Michael Sprenger,et al.  A global climatology of stratosphere–troposphere exchange using the ERA-Interim data set from 1979 to 2011 , 2014 .

[15]  M. Baldauf,et al.  Operational Convective-Scale Numerical Weather Prediction with the COSMO Model: Description and Sensitivities , 2011 .

[16]  S. Tibaldi,et al.  Cyclogenesis in the lee of the Alps: A case study , 1978 .

[17]  W. Newton,et al.  Extratropical Cyclones: The Erik Palmén Memorial Volume , 1990 .

[18]  Heini Wernli,et al.  Midstratospheric ozone variability over Bern related to planetary wave activity during the winters 1994–1995 to 1998–1999 , 2001 .

[19]  Heini Wernli,et al.  A Lagrangian analysis of stratospheric ozone variability and long‐term trends above Payerne (Switzerland) during 1970–2001 , 2002 .

[20]  R. Draxler An Overview of the HYSPLIT_4 Modelling System for Trajectories, Dispersion, and Deposition , 1998 .

[21]  Keith A. Browning,et al.  Organization of Clouds and Precipitation in Extratropical Cyclones , 1990 .

[22]  Sverre Petterssen,et al.  Motion and motion systems , 1956 .

[23]  Michael Sprenger,et al.  Balloon-borne match measurements of midlatitude cirrus clouds , 2013 .

[24]  Kenneth P. Bowman,et al.  Large-scale isentropic mixing properties of the Antarctic polar vortex from analyzed winds , 1993 .

[25]  Adrian F. Tuck,et al.  The calculation of stratospheric air parcel trajectories using satellite data , 2007 .

[26]  Harald Sodemann,et al.  Deuterium excess as a proxy for continental moisture recycling and plant transpiration , 2013 .

[27]  E. Danielsen,et al.  TRAJECTORIES: ISOBARIC, ISENTROPIC AND ACTUAL , 1961 .

[28]  Heini Wernli,et al.  An intercomparison of results from three trajectory models , 2001 .

[29]  R. J. Reed,et al.  A STUDY OF A CHARACTERISTIC TPYE OF UPPER-LEVEL FRONTOGENESIS , 1955 .

[30]  Sarah C. Jones,et al.  The impact of Typhoon Jangmi (2008) on the midlatitude flow. Part I: Upper‐level ridgebuilding and modification of the jet , 2013 .

[31]  Harald Flentje,et al.  Detailed modeling of mountain wave PSCs , 2003 .

[32]  Heini Wernli,et al.  A Lagrangian‐based analysis of extratropical cyclones. II: A detailed case‐study , 1997 .

[33]  Ying-Hwa Kuo,et al.  Thermal Structure and Airflow in a Model Simulation of an Occluded Marine Cyclone , 1992 .

[34]  Mark R. Schoeberl,et al.  A multiple‐level trajectory analysis of vortex filaments , 1995 .

[35]  R. Steinacker Airmass and frontal movement around the Alps , 1984 .

[36]  Louis W. Uccellini,et al.  A model-based diagnostic study of the rapid development phase of the Presidents' Day cyclone , 1988 .

[37]  Harald Sodemann,et al.  Interannual variability of Greenland winter precipitation sources: Lagrangian moisture diagnostic and North Atlantic Oscillation influence , 2008 .

[38]  Rüdiger Westermann,et al.  Three-dimensional visualization of ensemble weather forecasts – Part 2: Forecasting warm conveyor belt situations for aircraft-based field campaigns , 2015 .

[39]  Heini Wernli,et al.  The Milan photooxidant plume , 1997 .

[40]  A. Stohl Computation, accuracy and applications of trajectories—A review and bibliography , 1998 .

[41]  H. Wernli,et al.  A northern hemispheric climatology of cross‐tropopause exchange for the ERA15 time period (1979–1993) , 2003 .

[42]  A. Stohl,et al.  Interpolation Errors in Wind Fields as a Function of Spatial and Temporal Resolution and Their Impact on Different Types of Kinematic Trajectories , 1995 .

[43]  A. Buzzi,et al.  Study of high ozone concentrations in the troposphere associated with Lee cyclogenesis during Alpex , 1984 .

[44]  Michael Sprenger,et al.  Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies , 2009 .

[45]  John Methven,et al.  Estimating relationships between air mass origin and chemical composition , 2001 .

[46]  Sebastian Schemm,et al.  The Linkage between the Warm and the Cold Conveyor Belts in an Idealized Extratropical Cyclone , 2014 .

[47]  M. Garstang,et al.  Large-Scale Recirculation of Air over Southern Africa , 1996 .

[48]  Heini Wernli,et al.  An online trajectory module (version 1.0) for the nonhydrostatic numerical weather prediction model COSMO , 2013 .

[49]  Michael Sprenger,et al.  Swiss and Austrian Foehn revisited: A Lagrangian-based analysis , 2015 .

[50]  Mark Weeks,et al.  Foehn jets over the Larsen C Ice Shelf, Antarctica , 2014 .

[51]  Peter Clark,et al.  Conditional symmetric instability in sting‐jet storms , 2011 .

[52]  Harald Sodemann,et al.  Comparison of Eulerian and Lagrangian moisture source diagnostics - the flood event in eastern Europe in May 2010 , 2013 .

[53]  Raymond T. Pierrehumbert,et al.  Upstream Effects of Mesoscale Mountains , 1985 .

[54]  P. Jones,et al.  The Twentieth Century Reanalysis Project , 2009 .

[55]  Mark R. Schoeberl,et al.  The structure of the polar vortex , 1992 .

[56]  M. Facchini,et al.  The ABC-Pyramid Atmospheric Research Observatory in Himalaya for aerosol, ozone and halocarbon measurements. , 2008, The Science of the total environment.

[57]  Heini Wernli,et al.  Warm Conveyor Belts in the ERA-Interim Dataset (1979–2010): Part I: Climatology and Potential Vorticity Evolution , 2014 .