Revolutionizing the Future of Hydrological Science: Impact of Machine Learning and Deep Learning amidst Emerging Explainable AI and Transfer Learning
Rajib Maity,
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Aman Srivastava,
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Subharthi Sarkar
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et al.
Applied Computing and Geosciences,
Journal Year:
2024,
Volume and Issue:
24, P. 100206 - 100206
Published: Nov. 9, 2024
Language: Английский
Enhancing the prediction of irrigation demand for open field vegetable crops in Germany through neural networks, transfer learning, and ensemble models
Agricultural Water Management,
Journal Year:
2025,
Volume and Issue:
312, P. 109402 - 109402
Published: March 18, 2025
Language: Английский
Comparative analysis of machine learning models for rainfall prediction
Pritee Krishna Das,
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Rajiv Lochan Sahu,
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Prakash Chandra Swain
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et al.
Journal of Atmospheric and Solar-Terrestrial Physics,
Journal Year:
2024,
Volume and Issue:
264, P. 106340 - 106340
Published: Aug. 30, 2024
Language: Английский
Spatiotemporal variations and driving factors of evapotranspiration in the Yunnan-Guizhou Plateau from 2003 to 2020
S. Chen,
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Bo‐Hui Tang,
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Xianguang Ma
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et al.
Journal of Water and Climate Change,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Oct. 15, 2024
ABSTRACT
Evapotranspiration
(ET)
is
vital
for
the
Earth's
energy
and
water
balance,
particularly
influenced
by
global
climate
change.
The
Yunnan-Guizhou
Plateau
(YGP),
characterized
abundant
resources
intricate
terrain,
has
been
a
subject
of
study.
However,
previous
research
often
overlooked
intra-annual
variations
in
ET.
This
study
employed
high-spatiotemporal-resolution
ET
data
from
2003
to
2020
quantitatively
analyze
spatiotemporal
characteristics
on
YGP.
annual
showed
an
increasing
trend
0.18
mm/year,
with
monthly
increases
January,
March,
November,
December,
mainly
vegetation
transpiration,
which
accounts
56%
Breakpoints
trends
seasonal
components
occurred
January
2007
June
2018.
geodetector
model
assessed
impact
15
driving
factors
ET,
net
radiation
index
playing
dominant
roles
q-values
0.29
0.24.
Factor
impacts
varied
seasonally,
greater
influence
dry
season
(q-value
0.53
January)
less
rainy
0.08
August).
Pearson
correlation
analysis
indicated
that
different
months.
These
findings
enhance
understanding
plateau
responses
climate-change
mechanisms.
Language: Английский