Subversion Repositories lagranto.wrf

.TH trace

.SH NAME

.B trace - trace meteorological fields along trajectories

.SH SYNOPSIS

.B trace

.I inpfile

.I outfile

[

.I optional arguments

]

.SH DESCRIPTION

Trace meteorological fields along the trajectories given in the input file 

.I inpfile

and write a new trajectory file

.I outfile

. The meteorological fields to trace are listed in a 

.I

tracing file 

(default: tracevars). Partly they can be computed "online" (see ONLINE CALCULATIONS below), normally they are availbale on the primary and secondary P and S files.

.SH PARAMETERS

.TP 15

.I inpfile

input trajectory file; the appendix determines the format (see

.B reformat 

for details).

.TP 15

.I  outfile

output trajectory file; the appendix determines the format (see

.B reformat 

for details).

.SH TRACING FILE

Normally the meteorological fields for tracing are listed in a file with name 

.B "tracevars". 

The name of the tracing file can be changed with the optional argument "-v" (see below). The format of the tracing file is as follows:

.br

.TP 5

Format

.I field[:shift]

.I scale

.I computation 

.I prefix  

.TP 5

Shifts (optional)

.B - field:+100km[lat] 

- get field at trajectory position + 100 km shifted to north. A shift to south is obtained with field:-100km[lat].

.br

.B - field:+100km[lon] 

- get field at trajectory position + 100 km shifted to east. A shift to west is obtained with field:-100km[lon].

.br

.B - field:+2[dlat] 

- get field at trajectory position + 2 grid spacings dlat shifted to north. A shift to south is obtained with field:-2[dlat].

.br 

.B - field:+2[dlon] 

- get field at trajectory position + 2 grid spacings dlon shifted to east. A shift to west is obtained with field:-2[dlon].

.br 

.B - field:+50hPa 

- get field at trajectory position + 50 hPa shifted in vertical. A shift to lower pressures is obtained with field:-50hPa.

.br 

.B - field:+1dp 

- get field at trajectory position + 1 grid spacing DP shifted in vertical. A shift to lower pressures is obtained with field:-1dp. Note that DP is not fixed but varies with height.

.br 

.B - field:+6h 

- get field at trajectory position, but 6 h in the future. Shifts to the past are poeeible with field:-6h. In addition to hours (h), the time shift can be specified in minutes (min).

.TP 5 

Examples

.B - TH 1. 0 S : 

trace potential temperature (TH), scale it with 1 (no scaling); it is available on the S file (no computation is needed: 0).

.br

.B - Q 1000. 0 P :

trace specific humidity (Q), scale it with 1000 to have g/kg; it is available on the P file (no computation is needed: 0).

.br

.B - RH 1. 1 * :

trace relative humidity (RH), no scaling is needed (1.); relative humidity is not available on either P or S file and must be computed (1). 

.br

.B - TH:100hPa 1. 0 S :

As in the first example, but now the potential temperature is taken 100 hPa below the air parcel position.

.SH OPTIONAL ARGUMENTS

.TP 15

.TP 15

.I -i hours

time increments (in hours) for input P and  S files. If not explicitely specified, this is determined from the P and S files i

n the current directory.

.TP 15

.I -v varfile

Change the name of the tracing file from its default value "tracevars" to "varfile".

.TP 15

.I -f field scale

Trace field (with scaling scale) along the trajectories; the computation flag and the prefix for the data file is automatically set. This options allows the quick tracing of a field, without specifying a tracing file.

.TP 15

.I -changet

flag whether the times of the P and S files should be changed or not before a calculation; the default is that the

times are 

.B not 

changed. 

.TP 15

.I -noclean

flag whether parameter and criterion files should be kept; this is particularly helpful for debugging.

.TP 15

.I -timecheck

enforce a time check for the data file  

.SH SPECIAL INTERPOLATION MODES

.TP 15

.I -nearest

Do no interpolation between grid points; just take the nearest neighbor! This option is useful, if a discrete input field is given (e.g. labels), where interpolated values are meaningless.

.TP 15

.I -circle_avg radius

calculate area-weighted average over all grid points within a circle of the specified radius [km]. e.g. -circle_avg 200; note that the tracing of fields within a circle is quite slow.

.TP 15

.I -circle_max radius

calculate maximum within a circle of a radius [km]. e.g. -circle_max 200

.TP 15

.I -circle_min radius

calculate minimum within a circle of a radius [km]. e.g. -circle_min 200

.TP 15

.I -clustering

special mode to trace strat/trop label; the labels are attributed according to the program (tropopause), which clusters the atmosphere into five distinct classes according to the definition of the tropopause: PV (2 PVU) and potential temperature (380 K). The clustering mode is a refined version of the nearest mode, where all surrounding eight grid points vote for the final value.

.SH ONLINE CALCULATIONS

If the computation flag in the tracing file is set to 1, a meteorological field is calculated based upon the already traced fields and/or based on the fields on the primary and secondary P and S files. The following fields are implemented for online calculations:

.TP 5

.B - TH

potential temperature (in K).

.TP 5

.B - RHO

density (in kg/m^-3).

.TP 5

.B - RH

relative humidity (in %).

.TP 5

.B - THE

equivalent-potential temperature (in K).

.TP 5

.B - LHR

latent heating rate (K per input time step, typically K/6h). 

.TP 5

.B - D[U,V,T,TH]DX

horizontal derivative d[U,V,T,TH]/dx in west-east direction along pressure surfaces - zonal distance in m. U=zonal wind component (m/s), V=meridional wind component (m/s), T=temperature (deg C or K), TH=potential temperature (K). 

.TP 5

.B - D[U,V,T,TH]DY

horizontal derivative d[U,V,T,TH]/dy in south-north direction along pressure surfaces -meridional distance in m.  

.TP 5

.B - D[U,V,T,TH]DP

vertical derivative d[U,V,T,TH]/dp - pressure p in Pa.

.TP 5

.B - NSQ

squared Brunt-Vaisala frequence (in m^-2).

.TP 5

.B - RELVORT

relative vorticity (in s^-1) - RELVORT = DVDX - DUDY.

.TP 5

.B - ABSVORT

absolute vorticity (in s^-1) - ABSVORT = DVDX - DUDY + F, F being the Coriolis parameter.

.TP 5

.B - DIV

horizontal divergence of the velocity field (in s^-1) - DIV = DUDX + DVDY.

.TP 5

.B - DEF

horizontal deformation of the velocity field (in s^-1) - DEF = SQRT( ( DVDX + DUDY )^2 + (DUDX-DVDY)^2 ).

.TP 5

.B - PV

Ertel potential vorticity (in PVU) - PV = g * ( ABSVORT * DTHDP + DUDP * DTHDY - DVDP * DTHDX ).

.TP 5

.B - RI

Richardson number - RI = NSQ / (DUDP^2 + DVDP^2 ).

.TP 5

.B - TI

tubulence indicator according to Ellrod & Knapp - TI = DEF * SQRT( DUDP^2 + DVDP^2 ) * ( RHO * G).

.TP 5

.B - DIR

wind direction relative to zonal flow: (U,V)=(1,1) -> 45 deg; (U,V)=(1,-1) -> -45 deg; (U,V)=(-1,-1) -> -135 deg; (U,V)=(-1,1) -> 135 deg. A westerly flow has 0 deg, a southerly flow 90 deg, and a northerly one -90 deg. 

.TP 5

.B - DIST0

spherical distance (in km) from starting position.

.TP 5

.B - DIST

length of the trajectory (in km): integrated along great circle sections between the trajectory vertices.

.TP 5

.B - HEAD

heading of the trajectory: (DX,DY)=(1,1) -> 45 deg; (DX,DY)=(1,-1) -> -45 deg; (DX,DY)=(-1,-1) -> -135 deg; (DX,DY)=(-1,1) -> 135 deg. A path increment to east has heading of 0 deg; to the north 90 deg; to the south -90 deg; and to the west -180 deg. 

.SH EXAMPLES

.TP 5

.B [1] trace TRAJECTORY.1 TRAJECTORY.1 -changet

Read the trajectory file TRAJECTORY.1, trace all fields in the file "tracevars" along the trajectories and overwrite the existing trajectory file. In preparation, all times on the P and S files are changed prior to the tracing.

.TP 5

.B [2] trace INPTRA.1 OUTTRA.1 -f PV 1.

Trace PV (with scaling factor 1.) along the trajectories in trajectory file "INPTRA.1" and write a new trajectory file "OUTTRA.1".

.TP 5

.B [3] trace INPTRA.1 OUTTRA.1 -f PV:-100HPA 1.

As in example [2], but the PV is taken at a position 100 hPa higher (lower pressure) than the air parcel's position.

.TP 5

.B [4] trace INPTRA.1 OUTTRA.1 -f DIST0 1.

Get the spherical distance (in km) of the air parcel from its starting position.

.SH AUTHOR

Written by Michael Sprenger and Heini Wernli (January 2011).