Access the full text.
Sign up today, get DeepDyve free for 14 days.
Loading next page...
/lp/wiley/response-of-surface-energy-fluxes-and-hydrothermal-characteristics-to-hS7ubAasqi
References (75)
-
Li D. (2017)
The quantitative analysis of the hydro‐thermal dynamic of permafrost active layer effected by precipitationJournal of Arid Land Resources and Environmen, 31
-
K. Oleson, D. Lawrence, G. Bonan, B. Drewniak, M. Huang, C. Koven (2013)
Technical description of version 4.5 of the Community Land Model (CLM) -
Hirabayashi Y. (2013)
Global flood risk under climate changeNature Climate Change, 3
-
Lyu J. (2002)
A simulation study of atmosphere‐vegetation interaction over the Tibetan Plateau part II: net primary productivity and leaf area indexChinese Journal of Atmospheric Sciences, 26
-
Liu W. (1997)
Analysis on night‐rain agricultural climate resources in Xishuangbanna of ChinaJournal of Natural Resources, 12
-
H.‐O. Pörtner, D.C. Roberts, V. Masson‐Delmotte, P. Zhai, M. Tignor, E. Poloczanska (2019)
IPCC 2019: summary for policymakers. IPCC special report on the ocean and cryosphere in a changing climate -
Jiang J. (2020)
Study on the relationship between seasonal freezing‐thawing areas and summer precipitation in the Northern HemisphereJournal of Glaciology and Geocryology, 1
-
Gao Y. (2022)
The relationship between CO2 flux and vegetation leaf area index of four alpine grassland types in Qilian MountainsChinese Journal of Grassland, 44
-
Song Y. (2014)
Evaluation of simulation performance of land surface model NCARCLM4.5 at a degrated glassland station in semi‐arid areaTransactions of Atmospheric Sciences, 6
-
Yuan Y. (2019)
CLM4.5 model simulation of soil moisture over the Qinghai‐Xizang plateau and its performance evaluationChinese Journal of Atmospheric Sciences, 3
-
Luo S. (2020)
Freeze–thaw changes of seasonally frozen ground on the Tibetan Plateau from 1960 to 2014Journal of Climate, 33
-
Wang S. (2018)
Experiment studies on characteristics of surface‐to‐air exchange over the Southeast Tibet in ChinaJournal of Arid Land Resources and Environment, 2
-
Luo S. (2016)
Frozen ground temperature trends associated with climate change in the Tibetan Plateau Three River Source Region from 1980 to 2014Climate Research, 67
-
Wang Y. (2010)
Variation characteristics of meteorological elements in near surface layer over the Lulang Valley of southeastern Tibetan PlateauPlateau Meteorology, 1
-
Luo S. (2008)
Simulation analysis on land surface process of BJ site of central Tibetan Plateau using CoLMPlateau Meteorology, 27
-
Deng M. (2020)
Comparison of soil water and heat transfer modeling over the Tibetan Plateau using two community land surface model (CLM) versionsJournal of Advances in Modeling Earth Systems, 12
-
Wu B. (2014)
Land cover changes of China from 2000 to 2010Quaternary Sciences, 34
-
Swenson S.C. (2012)
Improved simulation of the terrestrial hydrological cycle in permafrost regions by the Community Land ModelJournal of Advances in Modeling Earth Systems, 4
-
Tang M. (1998)
Evidence that the “Big Gorge Bend” of the Yarlung Zangbo River is a “hot spot” on the earthScientia Sinica (Terrae), 5
-
Trenberth K.E. (1998)
Atmospheric moisture residence times and cycling: implications for rainfall rates and climate changeClimatic Change, 39
-
Ueno K. (2009)
Nighttime precipitation induced by a synoptic‐scale convergence in the central Tibetan PlateauJournal of the Meteorological Society of Japan. Ser. II, 87
-
Fang X. (2016)
A simulation and validation of CLM during freeze‐thaw on the Tibetan PlateauAdvances in Meteorology, 2016
-
Wang G. (2014)
Analysis on the features of energy budget on the complicated underlying surfaces in Southeast TibetPlateau and Mountain Meteorology Research, 4
-
Y. Gao, S. Jiang, Y. Zhang, J. Li, Z. Lin, X. Wu (1984)
Tibetan climate -
Yu Z. (2011)
Spatial and temporal variations of the night‐rain rate during summer over the Tibetan PlateauJournal of Mountain Science, 29
-
R.B. Stull (1988)
An introduction to boundary layer meteorology -
Hamm A. (2023)
Continentality determines warming or cooling impact of heavy rainfall events on permafrostNature Communications, 14
-
T. Stocker, D. Qin, G. Plattner, M. Tignor, S. Allen, J. Boschung (2013)
Climate change 2013: the physical science basis. Contribution of working group I to the fifth assessment report of the Intergovernmental Panel on Climate Change -
Chen Z. (2022)
Effects of different initial values on the simulation of permafrost hydrothermal processes at Xidatan Station on the Three‐River regionsPlateau Meteorology, 2
-
Ma X. (2005)
Precipitation variation characteristics and abrupt change over Qinhai‐Xizang Plateau in recent 40 yearsJournal of Desert Research, 1
-
Luo S. (2017)
Improving CLM4.5 simulations of land–atmosphere exchange during freeze–thaw processes on the Tibetan PlateauJournal of Meteorological Research, 31
-
Xu Z.X. (2010)
Decadal trend of climate in the Tibetan Plateau‐regional temperature and precipitationHydrological Processes, 22
-
D. Ye (1979)
Meteorology of Qinghai Tibet Plateau -
Li J. (2016)
Characteristics of land–atmosphere energy exchanges over complex terrain area of southeastern Tibetan Plateau under different synoptic conditionsChinese Journal of Atmospheric Sciences, 4
-
Dong Q. (2022)
Changes of precipitation and its effects on soil temperature and freeze‐thaw process in southeastern Xizang in recent 60 yearsPlateau Meteorology, 2
-
Gao D. (2008)
Expeditionary studies on the moisture passage of the Yarlung Zangbo RiverChinese Journal of Nature, 5
-
Wang X. (2018)
Precipitation over the Tibetan Plateau during recent decades: a review based on observations and simulationsInternational Journal of Climatology, 38
-
Z. Zhang (2021)
A big earth data platform for three poles -
Chen B. (2012)
On the origin and destination of atmospheric moisture and air mass over the Tibetan PlateauTheoretical and Applied Climatology, 110
-
Ma C. (2020)
Impact and sensitivity analysis of gravel parameterization on simulation of land surface processes on the Qinghai‐Xizang PlateauPlateau Meteorology, 6
-
Yu B. (2014)
Datasets of the boundary and area of the Tibetan PlateauActa Geographica Sinica, 69
-
Deng M. (2017)
Fluctuation of daily rainfall extreme in southeastern TibetJournal of Natural Disasters, 2
-
Douglas T.A. (2020)
Increased rainfall stimulates permafrost thaw across a variety of Interior Alaskan boreal ecosystemsnpj Climate and Atmospheric Science, 3
-
Kang Z. (2022)
Improving simulations of vegetation dynamics over the Tibetan Plateau: role of atmospheric forcing data and spatial resolutionAdvances in Atmospheric Sciences, 39
-
Yang K. (2011)
Response of hydrological cycle to recent climate changes in the Tibetan PlateauClimatic Change, 109
-
Chen L. (2020)
Influence of wintertime surface sensible heat flux variability over the central and eastern Tibetan Plateau on the East Asian winter monsoonClimate Dynamics, 54
-
Hu L. (2010)
Diurnal variability of precipitation depth over the Tibetan Plateau and its surrounding regionsAdvances in Atmospheric Sciences, 27
-
Xie Z. (2018)
Impact of the snow cover scheme on snow distribution and energy budget modeling over the Tibetan PlateauTheoretical and Applied Climatology, 131
-
Swenson S.C. (2012)
A new fractional snow‐covered area parameterization for the Community Land Model and its effect on the surface energy balanceJournal of Geophysical Research: Atmospheres, 117
-
Tan L.C. (2018)
High resolution monsoon precipitation changes on southeastern Tibetan Plateau over the past 2300 yearsQuaternary Science Reviews, 195
-
Immerzeel W.W. (2010)
Climate change will affect the Asian water towersScience, 328
-
Zhang M. (2021)
The effects of rainfall on the surface radiation of permafrost regions in Qinghai‐Tibet Plateau: a case study in Beiluhe areaJournal of Glaciology and Geocryology, 43
-
J. Du, J. Hu, Y. Zhang (2007)
The Tibetan agricultural climate resources -
Lawrence D.M. (2011)
Parameterization improvements and functional and structural advances in version 4 of the Community Land ModelJournal of Advances in Modeling Earth Systems, 3
-
Stull R.B. (1988)
10.1007/978-94-009-3027-8 -
Shi L. (2016)
The temporal‐spatial variations of soil moisture over the Tibetan Plateau during 1980–2012Journal of Glaciology and Geocryology, 5
-
Niu B. (2016)
Tower‐based validation and improvement of MODIS gross primary production in an alpine swamp meadow on the Tibetan PlateauRemote Sensing, 8
-
Kukulies J. (2020)
Temporal and spatial variations of convection, clouds and precipitation over the Tibetan Plateau from recent satellite observations. Part II: precipitation climatology derived from global precipitation measurement missionInternational Journal of Climatology, 40
-
Shi S. (2001)
Plant growth analysis of Kobresia humilis meadow community in Qingzang plateau regionsActa Ecologica Sinica, 21
-
Su Y. (2020)
Evaluation of simulated performance of CLM4.5 in alpine meadow over the Qinghai‐Xizang Plateau based on measured soil propertiesPlateau Meteorology, 6
-
Yang Y. (1987)
A preliminary study on the water Vapor Channel in the lower valley of the Yarlung Zangbo RiverScience in China, 8
-
Xu X. (2019)
Effect of the Asian Water Tower over the Qinghai‐Tibet Plateau and the characteristics of atmospheric water circulationChinese Science Bulletin, 64
-
Wang J. (2023)
Impact of thermally forced circulations on the diurnal cycle of summer precipitation over the southeastern Tibetan PlateauGeophysical Research Letters, 50
-
Tang X. (2015)
Analysis of the characteristics of radiation budget upon the complicated underlying surfaces in southeastern TibetJournal of Glaciology and Geocryology, 4
-
Li Y. (2009)
Characteristics of the precipitation over the eastern edge of the Tibetan PlateauMeteorology and Atmospheric Physics, 106
-
Luo S. (2009)
Soil thermal conductivity parameterization establishment and application in numerical model of central Tibetan PlateauChinese Journal of Geophysics, 52
-
Burns S.P. (2015)
The influence of warm‐season precipitation on the diel cycle of the surface energy balance and carbon dioxide at a Colorado subalpine forest siteBiogeosciences, 12
-
Byers H.R. (1949)
Measurement of rain temperatureJournal of Meteorology, 6
-
Wan G. (2017)
The precipitation variations in the Qinghai‐Xizang (Tibetan) Plateau during 1961–2015Atmosphere, 8
-
Wu G. (2007)
The influence of mechanical and thermal forcing by the Tibetan Plateau on Asian climateJournal of Hydrometeorology, 8
-
Xu X. (2008)
World water tower: an atmospheric perspectiveGeophysical Research Letters, 35
-
Sasaki T. (2003)
Drastic evening increase in precipitable water vapor over the southeastern Tibetan PlateauJournal of the Meteorological Society of Japan, 81
-
Yang K. (2018)
Improved simulation of frozen‐thawing process in land surface model (CLM4.5)Journal of Geophysical Research‐Atmospheres, 123
-
Chen B. (2012)
Simulation analysis on land surface process at Maqu Station in the Qinghai‐Xizang Plateau using Community Land ModelPlateau Meteorology, 6
-
Song J. (2020)
Modeling land surface processes over a mountainous rainforest in Costa Rica using CLM4.5 and CLM5Geoscientific Model Development, 13
- Publisher
- Wiley
- Copyright
- © 2024 Royal Meteorological Society
- ISSN
- 0899-8418
- eISSN
- 1097-0088
- DOI
- 10.1002/joc.8316
- Publisher site
- See Article on Publisher Site
Abstract
This study aimed to evaluate the applicability of the land‐surface model CLM 4.5 in the southeastern Tibetan Plateau by utilizing field observation data from Kabu and Pailong sites. Furthermore, the study investigated the impact of night‐time precipitation changes on radiation, surface energy fluxes and soil hydrothermal characteristics in this region. Results revealed that CLM 4.5 accurately simulated upward shortwave/longwave radiation, surface energy fluxes and soil temperature in this region. However, the simulation of soil moisture exhibited a slight fluctuation of the simulated value during precipitation, resulting in poorer performance during heavy precipitation and a failure to simulate the rapid change of latent heat flux and soil moisture. Sensitivity experiments demonstrated that night‐time precipitation significantly influenced upward shortwave/longwave radiation, energy budge and soil hydrothermal processes, with each element changing considerably with changes in precipitation. Surface energy fluxes and hydrothermal characteristics were found to be more sensitive to increased precipitation than decreased precipitation. Additionally, soil moisture was found to play a crucial role in the impact of precipitation changes on surface energy fluxes and hydrothermal characteristics. Furthermore, the study also found that changes in precipitation had a more pronounced effect on relatively dry areas and seasons than already extremely wet areas and seasons. Finally, the variation in soil moisture was found to be restricted by the original soil moisture. In conclusion, this study highlighted the significant influence of night‐time precipitation on surface hydrothermal characteristics and surface energy budget in the southeastern Tibetan Plateau.
Journal
International Journal of Climatology – Wiley
Published: Jan 1, 2024
Keywords: land‐surface model; sensitivity experiments; soil hydrothermal process; southeastern Tibetan Plateau precipitation