The Prague Post - Every 1C of warming means 15% more extreme rain, researchers say

EUR -
AED 4.114065
AFN 72.259582
ALL 90.790621
AMD 404.158249
ANG 2.004979
AOA 1027.255243
ARS 1706.277137
AUD 1.605841
AWG 2.019222
AZN 1.908846
BAM 1.955598
BBD 2.254667
BDT 138.445698
BGN 1.95798
BHD 0.422456
BIF 3355.553362
BMD 1.120234
BND 1.430852
BOB 13.181638
BRL 5.562192
BSD 1.119484
BTN 106.219027
BWP 15.421407
BYN 3.28696
BYR 21956.591821
BZD 2.251367
CAD 1.568609
CDF 2594.46299
CHF 0.92428
CLF 0.028243
CLP 1105.065844
CNY 7.480981
CNH 7.472639
COP 3552.732992
CRC 510.847228
CUC 1.120234
CUP 26.866225
CVE 110.25361
CZK 24.330933
DJF 199.339408
DKK 7.473811
DOP 68.662907
DZD 150.487454
EGP 61.701626
ERN 16.803514
ETB 182.080891
FJD 2.506193
FKP 0.837532
GBP 0.83759
GEL 2.901844
GGP 0.837532
GHS 12.979659
GIP 0.837532
GMD 82.897735
GNF 9906.976581
GTQ 8.557116
GYD 234.45578
HKD 8.78527
HNL 30.053895
HRK 7.537165
HTG 146.714844
HUF 366.731529
IDR 20269.350965
ILS 3.478944
IMP 0.837532
INR 106.361208
IQD 1697.024692
IRR 2052689.282929
ISK 136.422562
JEP 0.837532
JMD 177.661647
JOD 0.79429
JPY 175.72038
KES 145.354984
KGS 97.962924
KHR 4573.527541
KMF 492.347215
KPW 1008.210806
KRW 1482.658115
KWD 0.348046
KYD 0.932904
KZT 508.267495
LAK 25190.397759
LBP 100245.344367
LKR 371.711601
LRD 190.860284
LSL 18.546684
LTL 3.307761
LVL 0.677619
LYD 7.169259
MAD 10.995664
MDL 20.205913
MGA 5062.477032
MKD 61.598637
MMK 2352.70217
MNT 4032.758987
MOP 9.043866
MRU 44.738378
MUR 52.830672
MVR 17.319246
MWK 1941.099479
MXN 20.912986
MYR 4.576498
MZN 71.587148
NAD 18.546684
NGN 1492.219693
NIO 41.195744
NOK 10.482469
NPR 169.950444
NZD 1.961367
OMR 0.429016
PAB 1.119384
PEN 3.844503
PGK 5.013482
PHP 71.267107
PKR 309.775499
PLN 4.40251
PYG 6474.331183
QAR 4.080578
RON 5.3545
RSD 117.487863
RUB 89.990404
RWF 1653.929144
SAR 4.204519
SBD 9.045421
SCR 15.663382
SDG 673.825035
SEK 11.125947
SGD 1.430432
SHP 0.837151
SLE 25.709792
SLL 23490.757589
SOS 639.733914
SRD 42.152218
STD 23186.587781
STN 24.497469
SVC 9.794988
SYP 14565.285711
SZL 18.546084
THB 37.830725
TJS 10.315634
TMT 3.932022
TND 3.342755
TOP 2.697255
TRY 55.679905
TTD 7.606214
TWD 36.503734
TZS 2963.693842
UAH 50.679165
UGX 4931.490563
USD 1.120234
UYU 44.895362
UZS 13396.616091
VES 985.569686
VND 28949.654292
VUV 133.391269
WST 3.100456
XAF 655.957
XAG 0.020782
XAU 0.000280356799
XCD 3.02749
XCG 2.017492
XDR 0.792064
XOF 655.957
XPF 119.331742
YER 264.491333
ZAR 18.566461
ZMK 10083.456786
ZMW 22.506675
ZWL 360.71498
SSP 6436.51929
MXV 2.360302
  • BCC

    -0.5500

    77.74

    -0.71%

  • RIO

    -0.7200

    83.42

    -0.86%

  • GSK

    -0.4600

    50.75

    -0.91%

  • RBGPF

    2.6200

    72.77

    +3.6%

  • CMSC

    0.0000

    19.6

    0%

  • BCE

    -0.4100

    20.4

    -2.01%

  • JRI

    0.0700

    10.75

    +0.65%

  • RYCEF

    -1.7500

    15.26

    -11.47%

  • NGG

    -0.7800

    81.86

    -0.95%

  • CMSD

    0.1800

    19.78

    +0.91%

  • BTI

    -0.9900

    59.48

    -1.66%

  • RELX

    -0.0800

    40.54

    -0.2%

  • VOD

    -0.3800

    15.74

    -2.41%

  • AZN

    -1.0800

    171.49

    -0.63%

  • BP

    1.2700

    51.32

    +2.47%

Every 1C of warming means 15% more extreme rain, researchers say
Every 1C of warming means 15% more extreme rain, researchers say / Photo: Arif ALI - AFP/File

Every 1C of warming means 15% more extreme rain, researchers say

Global heating incrementally boosts the intensity of extreme rainfall at higher altitudes, putting two billion people living in or downstream from mountains at greater risk of floods and landslides, researchers said Wednesday.

Text size:

Every degree Celsius of warming increases the density of major downpours by 15 percent at elevations above 2,000 metres, they reported in the journal Nature.

On top of that, each additional 1,000 metres of altitude adds another one percent of rainfall.

A world, in other words, 3C hotter than preindustrial levels will see the likelihood of potentially devastating deluges multiply by nearly half.

The findings underscore the vulnerability of infrastructure not designed to withstand extreme flooding events, the authors warned.

Earth's surface has already warmed 1.2C, enough to amplify record-breaking downpours that put huge swathes of Pakistan under water last summer, and parts of California earlier this year.

On current policy trends, the planet will warm 2.8C by century's end, according to the UN's IPCC climate science advisory panel.

The new study -- based on data covering the last 70 years, and climate-model projections -- found two main drivers behind the upsurge in extreme rainfall events at altitude in a warming world.

The first is simply more water: scientists have long known that every 1C increase boosts the amount of moisture in the atmosphere by seven percent.

- From snow to rain -

Since the 1950s, heavy rainfall has become more frequent and intense across most parts of the world, according to the World Weather Attribution (WWA) consortium, which teases out the impact of climate change on specific extreme weather events, including heatwaves, droughts and tropical storms.

Extreme rainfall is more common and intense because of human-caused climate change in Europe, most of Asia, central and eastern North America, and parts of South America, Africa and Australia, the WWA has found.

The second factor uncovered by researchers was more surprising.

"This is first time that anyone has looked at whether those intense precipitation events fall as rain or snow," lead author Mohammed Ombadi, a researcher at Lawrence Berkeley National Laboratory in California, told AFP.

"Unlike snowfall, rainfall triggers runoff more rapidly, leading to a higher risk of flooding, landslide hazards and soil erosion."

Ombadi speculated that a higher rate of snow-turned-to-rain observed between 2,500 and 3,000 metres was due to precipitation at that altitude occurring a just below freezing.

The mountainous regions and adjacent flood plains likely to experience the biggest impacts from extreme rainfall events are in and around the Himalayas and North America's Pacific mountain ranges, according to the study.

The findings focused only on the northern hemisphere due to a lack of observational data from below the equator.

The regions most affected should prepare "robust climate adaptation plans," the authors said.

"We need to consider this increase in rainfall extremes in the design and building of dams, highways, railroads and other infrastructure if we want to make sure they will remain sustainable in a warmer climate," said Ombadi.

High-risk areas will either need to be avoided altogether, or built up with engineering solutions that can protect the communities living there, he added.

L.Hajek--TPP