Berliner Boersenzeitung - What is driving Europe's heatwave?

EUR -
AED 4.179607
AFN 72.258895
ALL 94.205288
AMD 419.32538
ANG 2.037333
AOA 1043.471931
ARS 1673.878652
AUD 1.646164
AWG 2.049676
AZN 1.931828
BAM 1.955918
BBD 2.296329
BDT 140.068478
BGN 1.924085
BHD 0.43002
BIF 3405.606125
BMD 1.137919
BND 1.476989
BOB 7.895478
BRL 5.920364
BSD 1.140164
BTN 107.948534
BWP 15.503938
BYN 3.202194
BYR 22303.209908
BZD 2.293039
CAD 1.616971
CDF 2577.385877
CHF 0.922079
CLF 0.026365
CLP 1037.657169
CNY 7.709175
CNH 7.735322
COP 3899.04488
CRC 517.224487
CUC 1.137919
CUP 30.15485
CVE 110.271674
CZK 24.228625
DJF 202.230987
DKK 7.475001
DOP 66.733159
DZD 152.068092
EGP 56.580855
ERN 17.068783
ETB 183.814318
FJD 2.561791
FKP 0.85899
GBP 0.86289
GEL 3.009787
GGP 0.85899
GHS 12.797775
GIP 0.85899
GMD 83.067764
GNF 9990.121794
GTQ 8.698526
GYD 238.534437
HKD 8.922706
HNL 30.504712
HRK 7.534161
HTG 149.069022
HUF 355.706046
IDR 20399.24405
ILS 3.40957
IMP 0.85899
INR 107.8111
IQD 1493.5904
IRR 1564638.450732
ISK 144.003725
JEP 0.85899
JMD 179.470074
JOD 0.806818
JPY 183.853426
KES 147.258242
KGS 99.511194
KHR 4575.854724
KMF 490.443242
KPW 1024.127384
KRW 1745.914618
KWD 0.351594
KYD 0.950158
KZT 554.603568
LAK 25248.528174
LBP 102099.879625
LKR 381.463088
LRD 207.502559
LSL 18.801338
LTL 3.359979
LVL 0.688316
LYD 7.316411
MAD 10.671146
MDL 20.072215
MGA 4763.288299
MKD 61.63521
MMK 2388.932514
MNT 4072.611663
MOP 9.207457
MRU 45.285348
MUR 54.57472
MVR 17.592561
MWK 1977.010972
MXN 20.012811
MYR 4.711558
MZN 72.710706
NAD 18.801338
NGN 1558.857449
NIO 41.952539
NOK 11.148254
NPR 172.716695
NZD 2.008275
OMR 0.437534
PAB 1.140169
PEN 3.859434
PGK 5.000325
PHP 69.924546
PKR 317.102593
PLN 4.285607
PYG 6950.390134
QAR 4.156252
RON 5.247057
RSD 117.351293
RUB 84.774961
RWF 1671.993851
SAR 4.273217
SBD 9.177362
SCR 15.231046
SDG 683.318583
SEK 11.088575
SGD 1.476194
SHP 0.849571
SLE 28.163574
SLL 23861.593974
SOS 651.636577
SRD 42.652585
STD 23552.623219
STN 24.500299
SVC 9.976604
SYP 125.77656
SZL 18.795138
THB 37.854581
TJS 10.57484
TMT 3.994095
TND 3.374904
TOP 2.739836
TRY 52.886538
TTD 7.741469
TWD 36.036527
TZS 2987.455785
UAH 51.179898
UGX 4173.252587
USD 1.137919
UYU 45.732768
UZS 13698.829126
VES 701.942638
VND 29955.714328
VUV 135.137568
WST 3.136474
XAF 655.993822
XAG 0.018439
XAU 0.000276
XCD 3.075283
XCG 2.054824
XDR 0.815849
XOF 655.993822
XPF 119.331742
YER 271.564061
ZAR 18.840509
ZMK 10242.636979
ZMW 20.453238
ZWL 366.409413
  • RBGPF

    -0.2700

    60.34

    -0.45%

  • BCC

    -0.6300

    71.91

    -0.88%

  • CMSC

    -0.0400

    22.12

    -0.18%

  • BCE

    0.3800

    23.03

    +1.65%

  • AZN

    3.6000

    180.03

    +2%

  • BTI

    1.8200

    60.72

    +3%

  • CMSD

    -0.1000

    21.98

    -0.45%

  • GSK

    1.2350

    51.975

    +2.38%

  • NGG

    0.7700

    81.74

    +0.94%

  • JRI

    -0.0100

    12.64

    -0.08%

  • RELX

    0.2600

    31.09

    +0.84%

  • RIO

    -3.4800

    95.88

    -3.63%

  • VOD

    -0.0850

    14.035

    -0.61%

  • BP

    -0.3940

    39.386

    -1%

  • RYCEF

    -0.1500

    18.25

    -0.82%

What is driving Europe's heatwave?
What is driving Europe's heatwave? / Photo: Christophe ARCHAMBAULT - AFP

What is driving Europe's heatwave?

Europe is baking under a scorching heatwave, with health warnings in place across western and central parts of the continent as temperatures climb to record-breaking highs.

Text size:

Among the factors driving these extremes are atmospheric and circulation patterns that keep hot air trapped in place for days, causing the mercury to slowly rise.

Scientists say these weather patterns are nothing new, but heatwaves are made more intense in a world hotter because of burning fossil fuels.

- 'Omega block' -

A circulation pattern over Europe is creating "the equivalent of a traffic jam in the atmosphere which locks in heat", Samantha Burgess from the European Centre for Medium-Range Weather Forecasts, told AFP.

A ridge of high pressure drawing hot air from North Africa is wedged between two areas of low pressure, one in central Europe and the other off the coast of Portugal.

This is known as an "omega block".

The pattern gets its name because the jet stream -- a current in the atmosphere that moves air and weather systems from west to east -- bends into a shape resembling the Greek letter.

- Vacuum cleaner -

The area of high pressure gets stuck "because of the pressure on either side", said Burgess, a climate scientist and strategic lead for climate at ECMWF.

"The jet stream gets stuck in a loop and it forces other weather systems to go around it," she said.

With little energy available to disrupt it, the omega pattern can persist for days -- or weeks -- allowing heat to stew and temperatures to intensify beneath it.

"So hence blocking -- it means that once this meteorological set-up gets going, it can just keep reinforcing itself for some time," said Will Lang, chief meteorologist at the UK's Met Office.

Sebastien Leas, a forecaster at France's weather service, likened it to a "vacuum cleaner, drawing in heat and masses of hot air rising from North Africa" and blasting it northward in a violent torrent.

- Heat dome -

If this pattern is very stable, the high pressure system can evolve into a "heat dome".

This acts like an atmospheric lid on a boiling pot, trapping heat beneath. Air sinking beneath the pressure warms as it is compressed, while heat near the surface cannot escape.

These conditions suppress cloud formation and favour still weather with little wind. Clearer skies allow more sunshine to cook Earth's surface, creating a heat feedback loop.

"Under the right conditions -- and you do need the right conditions -- it just gets hotter and hotter," said Lang.

- Hotter world -

Heat domes and omega patterns are nothing new and can form separately from each other, experts said.

A heatwave in late May across Europe was tied to a heat dome, while a horseshoe-shaped omega pattern was identified as a key driver of a major hot spell over France in June 2025.

They are also not unique to Europe but occur in both hemispheres across the world's middle latitudes. "They can occur over the Pacific, over Europe, over North America," said Burgess.

Scientists say there has been an increase in high pressure systems in Europe in recent decades but whether this is a consequence of climate change remains a subject of debate.

Burgess said when heat domes do occur "the subsequent heatwave is more intense than it otherwise would have been without climate change".

(Y.Yildiz--BBZ)