var description = [

// THERMAL PARAMETERS
//"",

// Thermal Updraft Velocity & B/S Ratio
"Kuvasta näet keskimääräisen noston voimakkuuden sekä alueen mihin keliä kehittyy. Normaali purjelentokeli tarkoittaa yleensä sitä, että noston voimakkuus on luokkaa 200 cm/s tai enemmän. Jos kuvassa näkyy tiheästi mustia pisteitä (B/S Ration), tuulen shear rikkoo nostoja tai tekee niistä puuskaisia.",

// Thermal Updraft Velocity (W*)
//"Kuvasta näet keskimääräisen noston voimakkuuden sekä alueen mihin keliä kehittyy. Normaali purjelentokeli tarkoittaa yleensä sitä, että noston voimakkuus on luokkaa 200 cm/s tai enemmän.",

// Buoyancy/Shear Ratio
//"Dry thermals may be broken up by vertical wind shear (i.e. wind changing with height) and unworkable if B/S ratio is 5 or less.  [Though hang-gliders can soar with smaller B/S values than can sailplanes.]  If convective clouds are present, the actual B/S ratio will be larger than calculated here due to the neglect of 'cloudsuck'.  [This parameter is truncated at 20 for plotting.]",

// Height of Critical Updraft Strength (Hcrit)
//"Korkeus, mihin kelvollinen nosto ulottuu, pilvi voi tosin tulla väliin.",

// Depth of Critical Updraft Strength (AGL Hcrit)
"Korkeus, mihin kelvollinen nosto ulottuu maasta laskien.",

// BL Top
//"Korkeus johon termiikki ulottuu.",

// BL Depth
//"Termiikin jylläyskerroksen paksuus.",

// Thermal Height Uncertainty
// "Noston ylärajan vaihtelevuus. Jos on esim 400 m ja korkeus mihin kelvollinen nosto (BL Top) ylettyy on 1600 m saattaa nostot käytännössä olla 1400-1800 m. ",

// MSL Height of max/min Wbl
//"Height at which the max / min of the vertical velocity in the Boundary Layer occurs, i.e. of \"BL Max Up/Down (Convergence)\" (qv)",

// Surface Heating                 
//"Heat transferred into the atmosphere due to solar heating of the ground, creating thermals.  This parameter is an important determinant of thermals strength (as is the BL depth).  This parameter is obtained directly from WRF model output and not from a BLIPMAP computation.",


// Normalized Surface Sun                 
"Paljonko pääsee auringonsäteilyä maanpinnalle suhteessa maksimiin, \"käänteinen\" pilvikartta.",

// Surface Temperature                 
"Lämpötila 2m korkeudella.",

// Surface Dew Point Temperature                 
//"Kastepiste 2m korkeudella.",

// WIND PARAMETERS
//"",

// MSL Pressure
// "Atmospheric Pressure at Mean Sea Level in mBar.",

// Surface Wind                 
"Tuuli 10m korkeudella, väri osoittaa voimakkuuden ja virtaviivat suunnan.",

// Boundary Layer Average Wind                 
//"The speed and direction of the vector-averaged wind in the BL.  This prediction can be misleading if there is a large change in wind direction through the BL (for a complex wind profile, no single number is an adequate descriptor!).",

// Wind at the Boundary Layer Top                 
//"The speed and direction of the wind at the top of the BL.  Speed is depicted by different colors and direction by streamlines.",

// Boundary Layer Wind Shear                 
//"The vertical change in wind through the BL, specifically the magnitude of the vector wind difference between the top and bottom of the BL.  Note that this represents vertical wind shear and does not indicate so-called 'shear lines' (which are horizontal changes of wind speed/direction).",

// BL Max. Up/Down Motion (BL Convergence)                 
"Nostavat alueet/jonot tai laskevat alueet eli Konvergenssi/Divergenssilinjat.",

// CLOUD PARAMETERS
//"",

// Cumulus Potential                 
//    "Kumpiaspotentiaali.",

// Cumulus Cloudbase (Sfc. LCL)                 
//    "Alimpien kumpupilvien pohjien korkeus, jos kumpiaisia on mahdollista syntyä.",
// Cumulus Cloudbase where CuPotential>0                 
    "Kaikki värilliset kohdat kartalla ovat alueita, joille syntyy kumpupilviä. Kumpupilven alarajan voi lukea värin perusteella. Kumpupilven alaraja riippuu maanpinnan lämpötilasta sekä kastepisteestä.",

// OvercastDevelopment Potential                 
//    "This evaluates the potential for extensive cloud formation (OvercastDevelopment) at the BL top, being the height difference between the BL CL (see below) and the BL top.  Extensive clouds and likely OD are predicted when the parameter is positive, with OD being increasingly more likely with higher positive values.  OD can also occur with negative values if the air is lifted up the indicated vertical distance by flow up a small-scale ridge not resolved by the model's smoothed topography.  [This parameter is truncated at -10,000 for plotting.]",

// OvercastDevelopment Cloudbase (BL CL)                 
//    "This height estimates the cloudbase for extensive BL clouds (OvercastDevelopment), if such exist, i.e. if the OvercastDevelopment Potential parameter (above) is positive.  The BL CL (Condensation Level) is based upon the humidity averaged through the BL and is therefore relevant only to extensive clouds (OvercastDevelopment) - unlike the above surface-based LCL which uses a surface humidity.  [This parameter is truncated at 22,000 for plotting.]",

// OvercastDevelopment Cloudbase where ODpotential>0                 
//    "Combining the previous two parameters, this depicts the OvercastDevelopment (OD) Cloudbase only at locations where the OD Potential parameter is positive.  This single plot can be used, instead of needing to look at both the OD Potential and OD Cloudbase plots, if the threshold OD Potential empirically determined for your site approximately equals the theoretical value of zero.",

// BL Explicitly-predicted CloudWater                 
//    "This parameter is primarily for DrJack's use.  It predicts the cloud base of extensive clouds based on model-predicted formation of cloud water, giving the lowest height at which the predicted cloud water density is above a criterion value within the BL.  In theory it should be useful predicting OvercastDevelopment (OD) within the BL since it predicts extensive cloudiness, i.e. when BL clouds are predicted to extend over a full model gridcell volume.  However, the criterion to be used to indicate the presence of clouds is problematical since no single value reliably differentiates between 'mist' and 'cloud' concentrations.  This parameter has not yet been verified again actual conditions - comparision to flight observations will be needed to evaluate its usefulness.",

// BL Cloud Cover
//    "This parameter provides an additional means of evaluating the formation of clouds within the BL and might be used either in conjunction with or instead of the other cloud prediction parameters.  It assumes a very simple relationship between cloud cover percentage and the maximum relative humidity within the BL.  The cloud base height is not predicted, but is expected to be below the BL Top height.  DrJack does not have a lot of faith in this prediction, since the formula used is so simple, and expects its predictions to be very approximate - but other meteorologists have used it and it is better than nothing.  Note: Since The the 'BL Cloud Cover', 'Cumulus Potential', and 'BL Extensive CloudBase' are based upon fundamentally different model predictions -- respectively the predicted maximum moisture in the BL, the predicted surface moisture, and an explicit cloud-water prediction -- they can yield somewhat differing predictions, e.g. the 'Cumulus Potential' can predict puffy cloud formation when the 'BL Cloud Cover' is zero or vice versa.",

// Rain
"Sadekertyma.",

// CAPE
"Kuuroherkkyys, arvot > 100 sadekuuroja, arvot > 500 ukkosta",

// WAVE PARAMETERS
"",

// Vertical Velocity at 850mb
"850mb korkeuden (n 1500m) pystynopeus ja tuulinuolet",

// Vertical Velocity at 700mb
"700mb korkeuden (n 3000m) pystynopeus ja tuulinuolet",

// Vertical Velocity at 500mb
"500mb korkeuden (n 5500m) pystynopeus ja tuulinuolet",

// Vert.Velocity Slice at Vert.Vel.Max
"Pystyleikkauskuva suurimman tuulen suuntaan",


// SOUNDINGS
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// "MODEL TOPOGRAPHY - - -",
""

// "Topography",
];