Shifted Flood and Ecology Regimes Due To Channel Bar Greening and Increased Flow Resistance in a Large Dammed River
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(20)
Published: Oct. 21, 2024
Abstract
Damming
profoundly
affects
downstream
flow‐sediment
regimes,
altering
channel
bar
dynamics
and
thereby
affecting
floods
riverine
biodiversity.
Here,
we
investigate
the
response
of
bars
to
upstream
damming
by
examining
patterns,
mechanisms,
impacts
in
Middle
Yangtze
River
(∼1,000
km).
Over
a
decade
post‐damming
observational
data
reveal
substantial
increases
revegetation
Leaf
Area
Index.
Shorter
flood
duration
stable
size
collectively
drive
greening.
Consequently,
denser
vegetation
has
slowed
flow
velocity
17%
±
2%
increased
resistance
21%
5%,
offsetting
water‐level
decrease
from
expansion
due
scouring
even
causing
slight
rise
floodwater
levels.
Furthermore,
markedly
altered
river
connectivity,
thermal
solute
dynamics,
detrimentally
fish
habitats
aquatic
life.
These
findings,
along
with
refined
stage
simulation
considering
flow‐sediment‐vegetation
interactions,
facilitate
sustainable
reservoir
operation
management
big
systems.
Language: Английский
Evolution of the Danube River’s islands on the Bulgaria-Romania border over the last century
PLoS ONE,
Journal Year:
2025,
Volume and Issue:
20(1), P. e0317711 - e0317711
Published: Jan. 30, 2025
The
border
line
between
Bulgaria
and
Romania
was
established
a
century
ago
on
the
Danube
River’s
thalweg,
going
around
islands.
Over
time,
islands
migrated;
to
avoid
conflicts,
located
are
declared
neutral
territory
by
both
countries
they
exit
from
use.
In
this
context,
paper
aims
draw
conclusions
spatial
dynamics
of
sandy
along
Bulgaria-Romania
border.
This
approach
is
mostly
GIS
work
various
documents
over
last
century,
with
interpretations
specific
fluvial
geomorphology.
Our
showed
patterns
evolution
(i)
trajectory
half
can
be
reconstituted
(i.e.,
merging
each
other
and/or
migrated).
redrawn
century.
form
dimensions
did
not
statistically
change
at
any
time
scale.
(ii)
At
scale
decades,
we
noticed
slow
formation
bars
lee
deposition
due
sediment
excess
then
migration
alluvial
until
an
island
or
bank,
followed
stabilization
vegetation
recruitment.
(iii)
Islands
their
migrated
countries’
line,
but
in
time.
invites
national
authorities
periodically
inventory
geomorphological
bars,
transfer
decision-making
process
for
stable
local
order
put
them
into
green
use
benefits
communities.
Language: Английский