# UK WEATHER & AIR QUALITY FORECASTING TEACHING PORTAL

## Product Descriptions

Contents

There are several types of products that are provided through ManUniCast. These fall in 4 differing categories: maps (both 2D and 3D), cross sections (both west to east and south to north), Skew-Ts, and meteograms. The description for these differing types of maps follow.

Many of these descriptions and definitions originate from the American Meteorological Society Glossary of Meteorology, which is located at this address: http://glossary.ametsoc.org/wiki/.

## Weather Products

### 2D Map

These maps are only plotted on one level, or are associated with the values at the surface.

Dewpoint:
The dewpoint temperature (in degrees Celsius) at 2m above the surface.
Level of Free Convection (LFC):
The height (in metres) at which an air parcel will rise without any additional forcing. From the level of free convection until the level which an air parcel returns to the environmental temperature the atmosphere is in a state of latent instability. A lower LFC can potentially indicate a more unstable atmosphere.
Lifting Condensation Level (LCL):
The height (in metres) at which an air parcel that has been lifted at the dry adiabatic lapse rate from the surface becomes saturated. A lower LCL indicates a moister atmosphere that may be more convective.
Maximum Convective Available Potential Energy (CAPE):
Amount of energy (in joules per kilogram) that is available to a rising air parcel. High values of CAPE can indicate a very unstable atmosphere. Typical values of CAPE in the United Kingdom for convective storms are less then 1000 J/kg, but can climb to values exceeding 3000 J/kg in the midwestern United States. CAPE can be defined as:
$$\mathrm{CAPE} = \int_{p_{n}}^{p_{f}}(\alpha_{p} - \alpha_{e})dp$$
where $$\alpha_{e}$$is the environmental specific volume profile, $$\alpha_{p}$$is the specific volume of a parcel moving upward moist-adiabatically from the level of free convection, $$p_{f}$$is the pressure at the level of free convection, and $$p_{n}$$is the pressure at the level of neutral buoyancy.
Maximum Convective Inhibition (CIN):
The amount of energy (in joules per kilogram) that is necessary to lift an air parcel from the surface to the level of free convection (LFC). Higher values of CIN indicate that convection may be less likely to form without sufficient upwards lifting caused by other atmospheric conditions. CIN can be defined as:
$$\mathrm{CIN} = -\int_{p_{i}}^{p_{f}}R_{d}(T_{vp} - T_{ve}) d \ln p$$
where $$p_{i}$$is the pressure at the level at which the parcel originates, $$p_{f}$$is the pressure at the LFC, $$R_{d}$$is the specific gas constant for dry air, $$T_{vp}$$is the virtual temperature of the lifted parcel, and $$T_{ve}$$is the virtual temperature of the environment.
A derived radar return (in dBZ) from the model microphysical information about cloud water and ice content. The simulated reflectivity is supposed to use the available information from the atmospheric model output to simulate what the return echoes would be for a United States WSR-88D Doppler radar, and the maximum simulated radar reflectivity is the highest value of that calculated radar return in a column of air.
Mixing Ratio (2D):
The ratio of the mass of water vapor in the atmosphere at that point to the mass of dry air. The 2D map gives the mixing ratio at 2 metres above the surface. Typically given in units of grams per kilogram (g/kg), or 1000 times the actual ratio.
Planetary Boundary Layer Height:
The height (in metres) of the atmospheric boundary layer, which forms the interface between the surface and the free atmosphere. A low boundary layer height can indicate an inversion in the atmosphere that prevents the air from mixing, therefore causing negative effects on air quality.
Potential Vorticity at 320 K:
Potential vorticity, in potential vorticity units (PVU, 1 PVU = 1.0 × 10-6 m2 s-1K kg-1) at the 320 K isotropic level.
Precipitable Water:
The amount of water vapor in a column of air if all of it was condensed into liquid and fell as precipitation. Typically given in values of either kg/m2 or mm.
Radar-derived rain rate at 1 km AGL:

This uses the simulated reflectivity at 1 kilometer above ground level to solve for R from this equation:

$$Z = 200 R^{1.6}$$

where $$Z$$ is the radar reflectivity factor and $$R$$ is the rain rate. This provides a field that can be compared easily to the radar rain rate composite found at the UK MetOffice (http://www.metoffice.gov.uk/public/weather/observations/?tab=map&map=Rainfall).

Relative Humidity (2D):
The ratio of the vapor pressure to the saturation vapor pressure for water. Typically given in values of percentage. The 2D map gives the mixing ratio at 2 metres above the surface.
Sea Level Pressure:
The atmospheric pressure at sea level (in hPa or mb). Since most station locations are at an elevation higher then sea level, the surface pressure at those station locations (or model grid points) are then reduced to what it would be if the model grid point was at sea level by assuming that the temperature at the model grid point would remain constant.
Simulated reflectivity at 1 km AGL:
A derived radar return (in dBZ) from the model microphysical information about cloud water and ice content. The simulated reflectivity is supposed to use the available information from the atmospheric model output to simulate what the return echoes would be for a United States WSR-88D Doppler radar.  The 1 km AGL simulated reflectivity interpolates the reflectivity field to 1 kilometer above ground level.
Snowfall depth (2D):
Total snow depth from model initialisation through plotting time (in metres). Snow height is calculated in the Noah land surface model based upon the compaction of a snowpack under conditions of increasing snow density. A full description of this process can be found in Koren (1999). Initial snow depths come from the GFS initial fields.

Koren, V. and Coauthors, 1999: A parameterization of snowpack and frozen ground intended for NCEP weather and climate models. J. Geophys. Res: Atmos., 104(D16), 2156–2202, doi: 10.1029/1999JD900232

Snowfall rate (2D):
Hourly snowfall in millimetres of liquid water equivalent. This field is the sum of the liquid water equivalents of all mixed phase or ice phase precipitation predicted by the Thompson microphysical parameterisation.
Temperature (2D):
The temperature (degrees Celsius) at 2 metres above the surface.
Total Accumulated Precipitation:
Precipitation from model initialisation through plotting time (in millimetres).
Wind Speed (2D):
The wind speed (in metres per second) at 10 metres above the surface.
Wind Vectors (2D):
Wind barbs of the 10 metre wind speed and direction. The wind barb points in the direction that the wind is coming from. A half-barb on the end indicates a 5 m/s wind speed, with a full barb a 10 m/s wind speed and a pennant 50 m/s wind speed.

### 3D Maps

These maps are plotted at multiple pressure levels throughout the atmosphere. These are standard pressure levels used throughout meteorology and are at 1000, 925, 850, 700, 500, 300, 250, and 200 hPa.

Absolute Vorticity:

The sum of the vorticity of the Earth (Coriolis parameter) and the relative vorticity. It is displayed in units of 10-5 s-1.

The relative vorticity can be defined as:

$$\zeta = \nabla \times \mathbf{u}$$

where $$\zeta$$ is the vorticity, $$\mathbf{u}$$ the velocity, and $$\nabla$$ the del operator.

The absolute vorticity can be represented by:

$$\eta = \zeta +f$$

where $$\eta$$ is the vertical component of the absolute vorticity vector, $$\zeta$$ is the relative vorticity, and $$f$$ is the Coriolis parameter.

Maxima in absolute vorticity indicate centers of rotation for large-scale weather systems within the atmosphere. Typically, absolute vorticity is viewed at 500 hPa in order to gauge the relative strength of the large-scale rotation of differing systems as well as the center of rotation in the middle of the atmosphere.

Equivalent Potential Temperature:
The temperature (in Kelvin) of an air parcel if it was brought down to the surface at the moist adiabatic lapse rate.
Geopotential Height:

The height (in metres) of a given point in the atmosphere in units proportional to the potential energy of unit mass (geopotential) at this height relative to sea level.

The relation between the geopotential height $$Z$$ and the geometric height $$z$$ is

$$Z = \frac{1}{980}\int_{0}^{z}gd{z}'$$

where $$g$$ is the acceleration of gravity. The two heights can nearly be considered the same in most meteorological purposes.

Layer Thickness from 1000 hPa:
The thickness (in metres) of the geopotential height (see above) from 1000 hPa to the selected atmospheric level. The layer thickness gives an idea about the average column temperature.  Low pressure centers due to their cold core structures will typically have a lower thickness then the surrounding atmosphere, although tropical storms have a warm core structure and therefore would higher thickness then the surrounding atmosphere.
Mixing Ratio (3D):
The ratio of the mass of water vapor in the atmosphere at that point to the mass of dry air. The 3D maps give the mixing ratio at the standard atmospheric levels. Typically given in units of grams per kilogram (g/kg), or 1000 times the actual ratio.
Moist Potential Vorticity:
Potential vorticity, in potential vorticity units (PVU, 1 PVU = 1.0 × 10-6 m2 s-1K kg-1) at various pressure levels throughout the atmosphere. Moist potential vorticity differs from potential vorticity due to use of equivalent potential temperature instead of potential temperature during its computation.
Potential Temperature:
The temperature of an air parcel (K) if it descended to the surface at the dry adiabatic lapse rate.
Potential Vorticity:
Potential vorticity, in potential vorticity units (PVU, 1 PVU = 1.0 × 10-6 m2 s-1K kg-1) at various pressure levels throughout the atmosphere.
Relative Humidity (3D):
The ratio of the vapor pressure to the saturation vapor pressure for water. Typically given in percentages (%). The 3D maps give the relative humidity at the defined pressure level.
Temperature (3D):
The temperature (in degrees Celsius) at the defined pressure level.
Vertical Velocity:
The wind speed (in metres per second) in the upwards (positive) or downwards (negative) directions at the defined pressure level.
Wind Speed (3D):
The wind speed (in metres per second) at the defined pressure level.
Wind Vectors (3D):
Wind barbs at the defined pressure level. The wind barb points in the direction that the wind is coming from. A half-barb on the end indicates a 5 m/s wind speed, with a full barb a 10 m/s wind speed and a pennant 50 m/s wind speed.

### Cross Sections

These plots are vertical slices of the atmosphere, either along 2 degrees west longitude or 53 degrees north latitude. This is meant to show how the weather systems proceed across the UK and also how they change with height. It can also give an idea of the depth of differing circulations. Several of the fields are reproduced from either the 2D or 3D maps, and their descriptions are repeated here.

Cloud Water Mixing Ratio:
The ratio of the mass of condensed water in the air to the total mass of the air. Typically given in units of grams per kilogram (g/kg), or 1000 times the actual ratio.
Cloud Ice Mixing Ratio:
The ratio of the mass of condensed ice in the air to the total mass of the air. Typically given in units of grams per kilogram (g/kg), or 1000 times the actual ratio.
Equivalent Potential Temperature:
The temperature (in Kelvin) of an air parcel if it was brought down to the surface at the moist adiabatic lapse rate.
Potential Temperature:
The temperature of an air parcel (K) if it descended to the surface at the dry adiabatic lapse rate.
Potential Vorticity:
Potential vorticity, in potential vorticity units (PVU, 1 PVU = 1.0 × 10-6 m2 s-1K kg-1) at various pressure levels throughout the atmosphere.
Relative Humidity:
The ratio of the vapor pressure to the saturation vapor pressure for water. Typically given in values of percentage. The cross sections give a vertical profile of the moisture present in the atmosphere.
A derived radar return (in dBZ) from the model microphysical information about cloud water and ice content. The simulated reflectivity is supposed to use the available information from the atmospheric model output to simulate what the return echoes would be for a United States WSR-88D Doppler radar.
Temperature (Cross section):
The temperature (in degrees Celsius) throughout the atmosphere.
Vertical Velocity (Cross section):
The wind speed (in metres per second) in the upwards (positive) or downwards (negative) directions.
Wind Speed (Cross section):
The wind speed (in metres per second) at the vertical cross section.
Wind Vectors (Cross section):
Arrows indicating the direction of the wind along the cross section.
Wind Streamline (Cross section):
Arrows indicating the trajectory of the wind along the cross section.

### Skew-Ts and Meteograms

Both Skew-T's and meteograms are point measurements, and are representative of the points given on this map:

Site ID Site Name
ABED Aberdeen, Scotland
ABER Aberporth, Wales
ALBE Albermare, Northumberland, England
ARRA Isle of Arran, Scotland
BHX Birmingham Airport (BHX), Scotland
CAMB Camborne, Cornwall, England
CAPD Capel Dewi, Wales
CARD Cardington, Bedfordshire, England
CBAY Castor Bay, Northern Ireland
CHIL Chilbolton Observatory, Hampshire, England
CWL Rhoose Cardiff-Wales Airport (CWL)
DALW Dalwhinney, Inverness-shire, Scotland
DUB Dublin Airport (DUB), Ireland
EDI Edinburgh Airport (EDI), Scotland
EGCT Cranfield Airport (EGCT), England
ESKD Eskdalemuir, Scotland, Scotland
EXT Exeter Airport (EXT), England
GLA Glasgow Airport (GLA), Scotland
GREN Royal Observatory, Greenwich, England
HERS Herstmonceux, Sussex, England
HOLM Holme Moss, West Yorkshire, England
INV Inverness Airport (INV), Scotland
LHR London/Heathrow (LHR), England
MAN Manchester Airport (MAN), England
MANX Isle of Man
NOTT Nottingham Weather Centre, England
NWI Norwich Airport (NWI), England
SCAF Scafell Pike, Cumbria, England
SNN Shannon Airport (SNN), Ireland
SYY Stornoway Airport (SYY), Scotland
TIRE Tireee, Argyll, Scotland
VALL Valley, Gwynedd, Wales
WHIT Whitworth Observatory, Manchester, England
WOOD Woodvale, Merseyside, England
YORK York, England

### Skew-Ts

A Skew-T log-P chart is a diagram of a profile of the atmospheric temperature, dewpoint, and wind speed. It is used to examine the vertical structure of the atmosphere at that grid point as well as to determine the stability of the air at that point.  A ManUniCast Skew-T gives several different forms of information at the top as well:

• PLCL - the pressure of the Lifting Condensation Level (hPa)
• TLCL - The temperature of the LCL (degrees C)
• Shox - Showalter Index, a stability index
• Pwat - The precipitable water in the column (cm)
• CAPE - the convectively available potential energy (J/kg).

### Meteograms

Meteograms show 78-hour plots of relative humidity (%), temperature (C), precipitation (mm), surface pressure (hPa), wind speed (m/s), and wind direction (degrees). These are meant to show the diurnal patterns over the 78-hour forecast cycle and represent the surface weather at the model grid point that is closes to the given location (as represented by the map above).

## Chemistry Products

### 2D & 3D Maps

Gas-phase Chemical Mixing Ratios:
For our atmospheric chemistry predictions (dchem) we plot mixing ratios of the following chemical compounds: ammonia (NH3), carbon monoxide (CO), dinitrogen pentoxide (N2O5), formaldehyde (HCHO), hydrogen peroxide (H2O2), nitrate radical (NO3), nitric oxide (NO), nitrogen dioxide (NO2), ozone (O3), peroxyacylnitrate (PAN), and sulpher dioxide (SO2). These mixing ratios are in parts per million by volume (ppmv), parts per billion by volume (ppbv) or parts per trillion by volume (pptv) (as denoted on the plots for each chemical compound). We also plot the mixing ratio of the sum of all non-methane volatile organic compounds (NM-VOC's) in ppbv, and the concentration of the hydroxyl radical (OH) in molecules per cubic centimetre of air.