The FAQ’s are no longer being updated. For more recent information, see the HYSPLIT Forum at: https://hysplitbbs.arl.noaa.gov/.
- HYSPLIT in General
- Running HYSPLIT on the READY Web Server
- Running HYSPLIT on your PC
- Volcanic Ash Model (currently HYSPLIT, formerly VAFTAD)
To find the answer to a question, click on the symbol.
HYSPLIT in General
- What meteorological archive data sets can I use to model Europe with HYSPLIT?
- What archived data are available on the web to run HYSPLIT with?
- What data is used to calculate the trajectories and what is the the vertical resolution of the data?
- I have a question about section five “meteorological input data” in the HYSPLIT_4 USER’s GUIDE. In page 49, what are the meanings of “pole latitude & longitude”, “reference latitude & longitude”, “synch latitude & longitude”, “synch point X and Y” and the relation (or difference) between “reference grid size” and “number X & Y points”? Or would you tell me what are their values if I have gridded meteorological data within lat. 5 N to 60 N and long. 110 E to 140 E., one degree resolution and I want to plot the back-trajectory within the same area?
- I am trying to better understand what the best approach is for calculating the HYSPLIT trajectories I need. I have mostly looked at using the EDAS data, but it has a lot of holes in it for the period I am interested in, so we wind up with trajectories truncated or not calculatable. I tried to fill in the holes with the FNL data. However, in one case when I calculated 120-hour backward trajectories from Potsdam, NY at 1800 on April 8, 1999 using both the EDAS and FNL data bases, I found that the EDAS data suggested the air was in the upper midwest 5 days prior, but the FNL put it into northern Quebec. Why the difference?
- Where can I find gridded meteorological data to simulate the Chernobyl accident?
- I have FNL meteorological files, which I use to compute trajectories with HYSPLIT. I need to extract the numerical value of some fields (geopotential at 700 hPa at each i,j grid point). I ran your program example which extracts the first field (precipitation), but I do not know how modify the program to extract geopotential at 700 hPa.
- I would like to extract surface winds from the archived EDAS data into ESRI Shape “shp” format, MapInfo “mif” format, or something similar. Is this possible?
- What archived data can I use prior to the start of the FNL dataset?
- Can I use surface observations in HYSPLIT?
- How do you parse GRIB files? NCAR/NCEP reanalysis data has all fields for a certain variable for an entire year in one large GRIB file. I’d like to extract (keeping the data in GRIB format) just one or several of the grid numbers from different files into one file containing all data for a given date/time. This is a requirement to run the ARL HYSPLIT converter to get the data in a format compatible with HYSPLIT. Does any one have a GRIB extractor or editor that allows one to parse grib files?
- I want to extract the u and v fields from the FNL archive according to the pressure level in some locations. Is this possible?
- Can HYSPLIT read other forms of meteorological data?
- I will be converting ECMWF grib files into ARL-packed format for use in calculating backward trajectories in Europe using your HYSPLIT model. What fields do I need to have for HYSPLIT to properly calculate my trajectories?
- How do I convert my ECMWF GRIB data files into ARL format using ecm2arl on the PC?
- Could you explain the equation (Zagl = ak2 + bk + c) used by HYSPLIT? What is the different between Ztop, Zgl, Zmsl and Zagl?
- My back trajectory run today looks different than the same trajectory I ran yesterday using the GDAS current7days archive. How often is the GDAS archive current7days file updated?
- Can I use WRF data with HYSPLIT?
- What principles are used for computing the mixing depth from the NCAR/NCEP reanalysis data?
- What is the smallest horizontal resolution allowed by the code, e.g., 10×10 meters, or 1×1 km?
Model Setup & Parameters
- Can HYSPLIT be setup to run a short-range dispersion calculation? If so, how?
- Which value should I input as the start height (MAGL)? What does “above model ground level” mean?
- I computed a vertical sounding at position (40.24, -3.40) with the FNL archived data. In the text results, the PRSS and the MSLP are 923.3 and 1021 mb, respectively. Assuming a hydrostatic atmosphere the model terrain height at this point can be estimated as 977 MASL. But in the text an Estimated Surface Height of 634 MASL is also reported, which is very close to the actual terrain height of 667 MASL. What should I consider as the model terrain height ASL at this point, 977 or 634 MASL?
- I have a question regarding what start height to make the trajectories and the correction factor for MAGL…
- If I choose AGL for the start height, does that mean that for the entire model run the computed heights are relative to the ground? I’m concerned about this because of the terrain in the mountains. I don’t want values to be “underground.”
- When I get backward trajectories starting at a rural East Coast site in NJ, which starting height(s) do you suggest is (are) appropriate? The terrain of the site is flat and near sea level. I am also wondering how long of a trajectory duration is recommended.
- I am attempting to calculate back trajectories for event based precipitation samples to trace sources of atmospheric pollutants (mercury, nitrogen, pesiticides). I am uncertain as to what height or pressure I should use in the model.
- If I know the in-situ measured SO2 concentration (pptv), corresponding location, altitude (4 km), and time of measurment, is it possible to calculate a back trajectory of that SO2 plume to know about the spreading over that source region?
- I’m interested in the backward trajectories at the costal site Baia Terra Nova, Antarctica, for aerosol studying. As in most of the Antarctic Plateau there are mountains, and I wonder if this is the reason why the meteorological model used by HYSPLIT “sees” the Antarctic continent so high (even though it is a coastal site)? Can I obtain backward trajectories at a lower height than the model terrain height (say at sea level), and if not, can I be confident in those trajectories starting from a much higher level than the level of the site under study?
- What would be the most accurate way to determine back trajectories (BT) for airmass sources at a particular field site. The sampling time at the field site was ~24 hours. Should I run a 24 hr BT for every hour during sampling? Would I then combine all of these BT’s to get an accurate BT for the airmass collected over the 24 hr sampling period? Also what height would you suggest to end the BT at, 10 m or 950 h Pa? (April 2004)
- Is terrain included in the HYSPLIT model and how accurate are surface trajectories computed for complex terrain?
- Is there anyway to change the simulation specification so that the concentration measurements are standardized across both:
- One location at different points in time and
- Different locations at the same point in time?
- Is the model designed only to model slow releases of chemicals or could it also be used in the case of explosions?
- Would HYSPLIT work to model an atmospheric release of a biological toxin?
- Can I run 1 trajectory every 6 hours every day for an extended period of time?
- Is there a batch job that can be submitted to the server to obtain 10-d back-trajectories for the time period specified?
- Is there a way to run multiple trajectories with a single command in hysplit?
- Is the time used to calculate trajectories UTC or local time?
Interpretation of Trajectory Results
- After calculating backward isentropic trajectories on the PC and looking at the plot, particularly the vertical motion plot at the bottom, I see motion across theta surfaces. My question is, shouldn’t I see vertical motion on a constant theta (potential temperature) surface?
- After calculating backward isobaric trajectories I see that the pressure is not constant and looking the vertical motion plot at the bottom of the plot, I see vertical motion (about 500m difference from the starting point to some other points ). Why is this?
- I am trying to do trajectory analysis for an event in which we have observed meteorological data. Is it possible to download HYSPLIT to the PC and feed it observed data from meteorological stations?
- When I ran a foward trajectory from a location on a previously computed backward trajectory, I did not return to the starting location of my backward trajectory. Why?
- Could you tell us how the precipitation rates are determined which accompany the air parcel trajectories in the tdump file?
- Is it possible to overlay several trajectories onto one map?
- How many trajectories can I draw in the same plot when I enter different names in trajectory Display GUI using a + symbol and what is the minimum number of tdump files which I need to create a cluster?
- How do I estimate the absolute (in km) and relative (%) errors when using the HYSPLIT trajectory model? Where does the error mostly come from (e.g., truncation error, interpolation error or wind field error)?
- What are the levels of uncertainty associated with back trajectory calculations in HYSPLIT?
- What are the levels of uncertainty associated with back trajectory calculations of ambient and potential temperature in the Hysplit model meteorological outputs? I am trying to use the model, to do 5-day backward trajectories of two air parcels (200m and 1000m) starting at my study location. I would like to use the temperature outputs to understand processes within my study region and would like to know its accuracy. (April 2004)
- How does HYSPLIT consider the vertical coordinate. If a trajectory meets the surface how does HYSPLIT work? Does it reflect, or use another method to solve it?
- We calculated three isentropic back trajectories simultaineously for the same latitude and longitude, but for three different altitudes. Then we calculated one back trajectory by itself. To my surprise the results are different. Why are the back trajectories different if you calculate them jointly or separately?
- Is the effect of the boundary layer considered when the model computes the trajectory?
- I have been running trajectories every hour for 24 hours to get a general idea of the airmass origin a single point during this period. Is there a way to obtain an average visual trajectory for a 24 hour period?
- Why are there small differences in my trajectories when I run more than one at a time versus running just one trajectory?
Interpretation of Concentration Results
- Is it possible to interpolate between two lines of equal concentration or between a maximum and a line?
- How is concentration defined in HYSPLIT and how does it relate to the radiation units of Bacquerel?
- Is there any way to obtain the concentration and deposition information in a data file instead of a graphic?
- When running HYSPLIT concentrations I got 10E-11 … 10E-17 for values of concentration. I understood that the unit is mass/m3.hr. My question is that in order to apply the numbers to total emission from a power plant stack, how can I calculate real plume concentration? Suppose it is 167381 ton/yr and converted 19 ton/hr, then, can I just multiply 19 ton/hr by 10E-11… to get real level?
- I found a case where there are deposition contours where there are no corresponding air concentration contours. Why?
Running HYSPLIT on the READY Server
- How do I calculate and visualize backward and forward trajectories for our air pollution monitoring station on the READY website?
- My research is to use wind trajectories to find pollutant sources in Chicago. How do I translate longitude and latitude into the exact location, say Sears Tower or United Center?
- What is the longest period over which trajectories can be calculated on the web?
- Is it possible to extract the the trajectory-data into an ascii-file?
- I am trying to do a backward trajectory for parcels involved in historical weather events, and I know that even minor changes in the point or time can yield much different results for the parcel origin. Is there a way to do an “ensemble” run, slightly perturbing the starting point?
- The model always gives a deposition plot. Can this influence the concentration plot? I mean: If you have a gas with no deposition at all, is the the concentration plot then still valid?
- Does HYSPLIT output 3 dimensional concentrations?
- How come when I use the back button on the browser, my settings to the HYSPLIT Model Setup form are returned to the default settings?
- Which datum do you use for the output from your models? NGVD 29? NAD27? NAD83? WGS84? Clarke Spheroid? And what does datum mean, anyway?
Running HYSPLIT on your PC
Downloading, Installing and Running the Model
- Where can I download the HYSPLIT PC version?
- What RAM and HD requirements are needed for running the trajectory and dispersion models on the PC?
- Is it necessary for the CONTROL file to be named “CONTROL”?
- How do you specify more than one meteorological file in the ‘set Meteo_file’ line of the Auto_traj.tcl script so the loop can run through many months of data?
- Can I produce the particle display on the PC version?
- Why do I get this message when trying to run PC Hysplit: “C:\hysplit4\guicode\hysplit4.tcl is not a valid Win32 application”?
- How do I run a BACKWARD trajectory using the PC version of HYSPLIT?
- When I ran a backward trajectory from a location on a previously computed forward trajectory, I did not return to the starting location of my forward trajectory. Why?
- Is there a way to run the model in “batch mode” that would generate trajectory endpoints?
- I am running a statistical program that groups hundreds of trajectories over one another and creates probability fields. My problem is that generating one trajectory at a time and converting the ASCII trajectory endpoint data into Excel format is far too time consuming. Is there a way to run a number of trajectories at once?
- An FAQ question under HYSPLIT in General explains how to adjust the start height to account for differences between model terrain and actual terrain. I’m assuming that it’s most accurate to use actual elevation plus my desired trajectory height as a starting height, and specify the option KMSL=1 in the setup.cfg file on the PC. Is this correct? Occasionally these trajectories are wildly different f rom those with KMSL=0 and the start height specified as meters above ground level.
- Is it possible to represent in the same map both forward and backward trajectories in order to make a comparision of the integration time step?
- For the web version of HYSPLIT, we can get temperature, potential temperature, precipitation, etc., along the trajectory. Can we do the same with the PC version?
- I purchased NCEP reanalysis GRIB data for summer 2001, downloaded the PC HYSPLIT model, and figured out how to convert the GRIB format to the HYSPLIT format using the compiled fortran program: ncr2arl. However, I am unsure about what latitude and longitude to input. I read that lat and lon are at the center of a 100×100 grid that is extracted from the GRIB file. So if my study area is around the North Eastern Pacific/West Coast of the US, should I just input my center lat and lon from my study area? I am trying to do backward air parcel trajectories of the marine atmospheric air located off Oregon. I am worried that if the grid extracted is only 100×100 from my center lat/lon that long duration backward trajectories might cover a larger area than the grid extracted. How should I deal with this? Finally, when using display.exe (or HYSPLIT GUI interface) to display contour maps, should I again enter the center lat/lon of my study area (in other words is the diplay.exe plotting the extracted 100×100 grid?) and what is meant by the radius (degLat)? What value of radius should I put in and how does different values change my contour map?
- When I set up a matrix run and have the heights specified at a certain altitude (using MSL), why do the results show the starting points at different heights instead of at a constant one? (April 2004)
- Please let me know is it possible to classify the trajectories by cluster analysis and draw a mean trajectory of each cluster using the PC version of Hysplit.
- The model prints on a large scale (all of Europe), while the concentration area itself is sometimes rather small. Is it perhaps possible to reduce the scale of the map?
- I have several months of the EDAS data files on my PC and wish to run several months at one time. Is there a way to run the model in “batch mode” that would generate deposition and concentration for each endpoint?
- I downloaded the latest version of HYSPLIT for the PC. How do I run the dispersion simulation backwards? I tried a negative number of hours run time, as for backward trajectories, but I got the same result as with positive number of hours.
- I am trying to run HYSPLIT (PC version) for Mercury (emit in gas phase). For chemical depositon set up, the model asks f or Surface Reactivity Ratio, Diffusivity Ratio, and Effective Henry’s Constant. At this time I could not find any of the se properties for (Hg+2 or HgO). I wonder is there anyone who did this pollutant simulation before. Any suggestion about where to obtain this information would be appreciated.
- I am looking to run concentrations for about 300 plants in HYSPLIT for use in an econometric analysis. I am running the concentration model for each plant and producing a GIS map for each model output. My problem is that generating one concentration and one GIS map at a time is very time-consuming and I am wondering if there is a way to do all 300+ of the concentrations at the same time? I want the model (time, pollutant characteristics, etc.) to be all the same for each model run, the only difference is the emission source and the height.
- How do I calculate deposition?
- I am using the PC version of the model on a Windows NT computer and am having trouble running it. I downloaded some archived files from the ftp site, and when I ask the model to use them I get the following error:HYSPLIT4 (Dec 98) – Initialization
Unable to find file: JUN98.BIN
On local directory : C:/HYSPLIT4/METDATA
Check input CONTROL file for correct values
Stop – Program terminated.I edited the control file by taking out the relative reference pathfile and put in the specific fully qualified directory path C:/hysplit4/metdata/ Do you have any suggestions on how to correct this problem?
- I purchased FNL meteorological files from NCDC for 1998, and they sent me a tape with the files. When I run the HYSPLIT model however, I get the following message:
- I have been quite successful running the trajectories off the website, but have not been able to get the downloaded software to work correctly. It seems to put out the default example graph every time, even after other meteorological data has been entered. Since I have been using HYSPLIT on the web, it doesn’t really matter. But I was wondering if the website accesses the hard drive, or if the software is actually not necessary and the website can be used instead? Are there things I can do using the software that are not available on the web? If so, what?
- Why can’t I run a back trajectory from 1900 UTC on 31 July, 2001 using downloaded FNL data? I attached my CONTROL file for you.
- When using trajplot.exe to plot multiple HYSPLIT output files, we are having trouble getting trajplot to recognize output files unless they are named tdump, tdump1, tdump2, …, tdumpn. Is it necessary for the file name to contain “tdump”?
- I am trying to calculate trajectories using my own MM5 output files. I compiled the mm5toarl routine and created the arl formatted files compatible with HYSPLIT, but it still doesn’t work. I used the chk_file program and there is an error with the header. Should I change something in the mm5toarl routine?
- I am attempting to run the HYSPLIT model daily for a 10 year period. I received the error message:
"*ERROR* runset: Numb meteo grids exceed DEFGRID limit - 12"
Is there a restriction of the length the model can run for? If so how do I get around this or do I have to restrict it to a single year?
- I have been trying to use the convert program to trim the white space around the edge of the hysplit plots using the ImageMagik ‘convert -trim’ command. This seems to have no effect on the image. The ‘-crop IxJ’ option has limited success. Is this an underlying issue with the .ps files that trajplot and concplot create?
- I received the following error. What could be wrong?
> > Model started ... > HYSPLIT48 (March 2007) - Initialization > Calculation Started ... please be patient > *ERROR* metpos: start point not within (x,y,t) any data file > xp,yp : 7.800000 12.60000 > time (min) : 53864640
- Why are the results different for the same run on the web versus the PC?
- When I “Run Standard Model” after saving the “Trajectory Setup”, I get a static message
> Model started ... > HYSPLIT48 (February 2008) - Initialization
This does not change. Why?
Volcanic Ash Model (currently HYSPLIT, formerly VAFTAD)
- As an airline pilot I always check the volcanic ash dispersion forecasts for Colima and Popoctptl whenever I fly Toronto-Mexico City, however I’m a little uncertain as to just how much gravity I should treat them with. If I was flying, say, from Miami to Mexico City at 18000ft can you tell me just what I might encounter if VAFTAD has a big red “blotch” along my route? Should I be planning to avoid it altogether or is the ash likely to be too dissipated to cause a problem?
- The HYSPLIT distribution models will often show significant areal coverage. Is there a threshold particle density that defines the plume boundaries and if so, is it one that corresponds to a known aircraft danger/non-danger threshold ?
- I am doing a project on air pollution due to Volcanic activity. I am missing one major part of the project: a model for the plume so that I can calculate the contaminant dispersion. I was wondering if one of you were familiar with such models and if I could get any information about them.
- Is it true that the VAAC’s do not issue volcanic ash dispersion model forecasts (sometimes called VAFTADs using the name of an earlier model), but use them as guidance, like the PUFF and AVHRR? If I wanted to see your forecast, then would need to look up your bulletin and the attached VAAC chart along with the SIGMETS bulletin, or do you send the VAFTAD out as a graphic?
- I saw a program on TV that stated volcanic gas and/or ash is necessary for earth’s healthy atmosphere, and that volcanic erruptions cause a protective layer between us and the sun. Is this in fact true?
- Volcanic Ash
- Smoke Forecasting
- Smoke: Prescribed Burns
- Inverse Modeling
- Inline WRF-HYSPLIT Coupling
- DATEM Evaluation