Table 1 shows the number of examples of each Grosswetterlagen circulation type represented in the ACCORD datasets. This shows that all circulation types are adequately represented, although some circulation types occurr far more frequently than others.
Grosswetterlagen | Description | Examples |
Wa | West anticyclonic | 681 |
Wz | West cyclonic | 1767 |
Ws | Southern West | 283 |
Ww | Angleformed West | 213 |
SWa | Southwest anticyclonic | 325 |
SWz | Southwest cyclonic | 366 |
NWa | Northwest anticyclonic | 265 |
NWz | Northwest cyclonic | 479 |
HM | Central European high | 602 |
BM | Central European ridge | 1133 |
TM | Central European low | 265 |
Na | North anticyclonic | 92 |
Nz | North cyclonic | 312 |
HNa | North, Iceland high, anticyclonic | 225 |
HNz | North, Iceland high, cyclonic | 201 |
HB | British Isles high | 372 |
TrM | Central European trough | 488 |
NEa | North-East anticyclonic | 153 |
NEz | North-East cyclonic | 175 |
HFa | Fennoscandian high anticyclonic | 367 |
HFz | Fennoscandian high cyclonic | 207 |
HNFa | Norwegian Sea - Fennoscandian high anticyclonic | 167 |
HNFz | Norwegian Sea - Fennoscandian high cyclonic | 184 |
SEa | Southeast anticyclonic | 232 |
SEz | Southeast cyclonic | 145 |
Sa | South anticyclonic | 197 |
Sz | South cyclonic | 78 |
TB | British Isles low | 267 |
TrW | Western European trough | 560 |
U | Unclassifiable | 157 |