The Lagrangian analysis tool LAGRANTO - version 2.0

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. Trajec5 tory 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 10 potential vorticity (PV) greater than 2 PVU). 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 quasi15 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 20 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]  Mark R. Schoeberl,et al.  A reinterpretation of the data from the NASA Stratosphere‐Troposphere Exchange Project , 1995 .

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

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

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

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

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

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

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

[10]  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 .

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

[12]  H. Synal,et al.  On the origin of 129I in rain water near Zürich , 2001 .

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

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

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

[16]  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 .

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

[18]  T. Flury,et al.  Water vapor transport in the lower mesosphere of the subtropics: a trajectory analysis , 2008 .

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

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

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

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

[23]  Rüdiger Westermann,et al.  3-D visualization of ensemble weather forecasts – Part 2: Forecasting warm conveyor belt situations for aircraft-based field campaigns , 2015 .

[24]  Sverre Petterssen,et al.  Weather analysis and forecasting , 1940 .

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

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

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

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

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

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

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

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

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

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

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

[36]  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 .

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

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

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

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

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

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

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

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

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

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

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

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

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

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

[51]  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.

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