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Ni Dai
Observed name:
Dai, Ni
Institution:
University of California, Los Angeles
Observed institutions:
University of Miami,
University of California, Los Angeles,
Earth System Science Interdisciplinary Center,
University of Maryland, College Park
ORCID:
0000-0001-9973-0561
Observed ORCID:
0000-0001-9973-0561
OpenAlex ID:
A5063224424
Model spread in tropical low cloud feedback tied to overturning circulation response to warming
2022
·
Kathleen A. Schiro
, Hui Su
, et al.
·
Nature Communications
·
36
PDF
Twentieth century ENSO-related precipitation mean states in twentieth century reanalysis, reconstructed precipitation and CMIP5 models
2016
·
Ni Dai
, Phillip A. Arkin
·
Climate Dynamics
·
14
Convective Aggregation and the Amplification of Tropical Precipitation Extremes
2020
·
Ni Dai
, Brian J. Soden
·
AGU Advances
·
12
PDF
Evaluation of CloudSat Radiative Kernels Using ARM and CERES Observations and ERA5 Reanalysis
2021
·
Ni Dai
, Ryan J. Kramer
, et al.
·
Journal of Geophysical Research Atmospheres
·
2
PDF
Diagnosis of ENSO-related precipitation changes during the twentieth and twenty-first centuries using reanalyses and two multi-model clusters
2020
·
Ni Dai
, Phillip A. Arkin
·
Climate Dynamics
·
2
Observed Links Between Atmospheric Cloud Radiative Effects and Mesoscale Organization of Deep Convection
2025
·
Ni Dai
, Hui Su
, et al.
·
Journal of Geophysical Research Atmospheres
PDF
Diabatic Heating Differences in ERA-Interim, MERRA-2, and CFSR Atmospheric Reanalyses, and Intercomparison of the Reanalyses and CMIP5 ENSO Heating Distribution
2018
·
Ni Dai
·
98th American Meteorological Society Annual Meeting
El Niño Southern Oscillation and Related Precipitation in Recent Atmospheric Reanalyses and Cmip5 Model Simulations
2018
·
Dai, Ni
·
University Libraries (University of Maryland)
ENSO-related Precipitation Seasonal Evolution and Multi-decadal Changes in Recent Reanalysis Datasets and CMIP5 Models
2015
·
Ni Dai
, Phillip A. Arkin
·
2015 AGU Fall Meeting
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Works count:
9
Citation count:
66
H-index:
3
I10-index:
3
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