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[PDF] Top 20 Evaluation of global continental hydrology as simulated by the Land surface Processes and eXchanges Dynamic Global Vegetation Model

Has 10000 "Evaluation of global continental hydrology as simulated by the Land surface Processes and eXchanges Dynamic Global Vegetation Model" found on our website. Below are the top 20 most common "Evaluation of global continental hydrology as simulated by the Land surface Processes and eXchanges Dynamic Global Vegetation Model".

Evaluation of global continental hydrology as simulated by the Land surface Processes and eXchanges Dynamic Global Vegetation Model

Evaluation of global continental hydrology as simulated by the Land surface Processes and eXchanges Dynamic Global Vegetation Model

... the continental hydrological cycle. Here the model is assessed for its ability to simulate large-scale spatial and temporal runoff patterns, in order to test its suitability for modelling future ... See full document

15

Evaluation of the snow regime in dynamic vegetation land surface models using field measurements

Evaluation of the snow regime in dynamic vegetation land surface models using field measurements

... ing land surface ...known land surface models, infer fresh snow density and snow density evolution, quantify the effects of uncertainties in SWE on simulated soil temperatures, and test ... See full document

17

The effect of GCM biases on global runoff simulations of a land surface model

The effect of GCM biases on global runoff simulations of a land surface model

... UK Land Environment Simulator (JULES) model (Best et ...based model that calculates water, energy, and carbon exchanges between the land sur- face and the ...the model are ... See full document

23

Modifying a dynamic global vegetation model for simulating large spatial scale land surface water balances

Modifying a dynamic global vegetation model for simulating large spatial scale land surface water balances

... river hydrology in the ...These processes contributed to overestimation of discharges for large rivers, such as the Murray River and Blue Nile River, in arid regions ...satellite-based land cover and ... See full document

19

LPJmL4 – a dynamic global vegetation model with managed land – Part 1: Model description

LPJmL4 – a dynamic global vegetation model with managed land – Part 1: Model description

... evaluate model performance for processes ...to simulated vegetation and carbon cy- cle dynamics (Bondeau et ...Earth’s land surface offers new possibilities for ... See full document

33

LPJmL4 – a dynamic global vegetation model with managed land – Part 2: Model evaluation

LPJmL4 – a dynamic global vegetation model with managed land – Part 2: Model evaluation

... This global dataset is based on a larger set of eddy flux tower measurements than the dataset of Luyssaert et ...empirical model based on operational re- mote sensing data by the Moderate Resolution Imaging ... See full document

27

ORCHIDEE-PEAT (revision 4596), a model for northern peatland CO 2, water, and energy fluxes on daily to annual scales

ORCHIDEE-PEAT (revision 4596), a model for northern peatland CO 2, water, and energy fluxes on daily to annual scales

... This model was applied at Mer Bleue Bog in southern Canada and validated with data from peat-core ...mulation model that works at an annual time step but can- not simulate seasonal variations of key water ... See full document

23

Implementing the nitrogen cycle into the dynamic global vegetation, hydrology, and crop growth model LPJmL (version 5.0)

Implementing the nitrogen cycle into the dynamic global vegetation, hydrology, and crop growth model LPJmL (version 5.0)

... dynamical global vegetation, hydrology, and crop growth model LPJmL is extended with a terrestrial nitrogen cycle to account for nutrient limita- ...particular, processes of soil ... See full document

24

Implementation and evaluation of a new methane model within a dynamic global vegetation model: LPJ-WHyMe v1.3.1

Implementation and evaluation of a new methane model within a dynamic global vegetation model: LPJ-WHyMe v1.3.1

... between vegetation, hydrology, soil thermal regime and methane-related processes is ...from global wetlands (Cao et ...the dynamic interactions between hydrol- ogy, soil temperature, ... See full document

20

Improved simulation of fire–vegetation interactions in the Land surface Processes and eXchanges dynamic global vegetation model (LPX-Mv1)

Improved simulation of fire–vegetation interactions in the Land surface Processes and eXchanges dynamic global vegetation model (LPX-Mv1)

... of vegetation changes and carbon seques- tration in response to future climate-induced changes in fire ...However, simulated NR ecosystem re- covery is slower than observations ...the model does not ... See full document

23

Impact of model developments on present and future simulations of permafrost in a global land-surface model

Impact of model developments on present and future simulations of permafrost in a global land-surface model

... The simulated permafrost in JULES is shown in ...the model developments brings in much more spatial variability in ALT, which generally matches with the patterns of continuous/discontinuous ...the ... See full document

17

On the sources of global land surface hydrologic predictability

On the sources of global land surface hydrologic predictability

... Hydrologic predictability at seasonal lead times (1 to 6 months) is derived from knowledge of initial hydrologic conditions (IHCs), which includes soil moisture (SM), snow water content (SWE), ground water and ... See full document

16

Analysis fire patterns and drivers with a global SEVER-FIRE v1.0 model incorporated into dynamic global vegetation model and satellite and on-ground observations

Analysis fire patterns and drivers with a global SEVER-FIRE v1.0 model incorporated into dynamic global vegetation model and satellite and on-ground observations

... between land use and timing of pyrogenic activities in SEVER would possi- bly also extend to a better representation of fire ...and land management prac- tices (Clerici et ...of land use in a ... See full document

22

Simulated Lightning in a Convection Permitting Global Model

Simulated Lightning in a Convection Permitting Global Model

... previous global lightning simulation, Finney et ...in global models, the diurnal peak in convection is around local noon (Birch et ...major continental regions is observed to peak in the afternoon ... See full document

8

Modeling forest plantations for carbon uptake with  the LPJmL dynamic global vegetation model

Modeling forest plantations for carbon uptake with the LPJmL dynamic global vegetation model

... managed land to natural forest between 2015 and 2100 re- sults in additional C uptake of 16 and 37 PgC by 2065 and 2100, ...limit global warming to 2 ◦ C for a range of scenarios in which both the start ... See full document

14

Representing nighttime and minimum conductance in CLM4.5: global hydrology and carbon sensitivity analysis using observational constraints

Representing nighttime and minimum conductance in CLM4.5: global hydrology and carbon sensitivity analysis using observational constraints

... CLM4.5SP model used here is an updated ver- sion of ...radiation, surface wind speed, specific humidity, and air pressure from 1901 through 2010, and did not include the in- fluences of nitrogen deposition, ... See full document

11

ASSESSING THE SURFACE ENERGY BALANCE COMPONENTS IN THE SNAKE RIVER BASIN

ASSESSING THE SURFACE ENERGY BALANCE COMPONENTS IN THE SNAKE RIVER BASIN

... irrigated model runs with non-irrigated model runs and the differences (irrigated – non-irrigated; I-NI) were ...in surface (skin) temperature (first column) and soil moisture (second column) at the ... See full document

180

ERA Interim/Land: a global land surface reanalysis data set

ERA Interim/Land: a global land surface reanalysis data set

... the land surface model, and (iii) the lack of data as- similation of snow depth in ...snow model lead predominantly to differences in the marginal snow areas and seasonal ...the model ... See full document

19

The representation of root processes in models addressing the responses of vegetation to global change

The representation of root processes in models addressing the responses of vegetation to global change

... of vegetation reflectance by using the normalized-difference vegetation index ...temperate vegetation, with the largest increases across the northern ...that vegetation is becoming more leafy ... See full document

11

Comparison of different sequential assimilation algorithms for satellite-derived leaf area index using the Data Assimilation Research Testbed (version Lanai)

Comparison of different sequential assimilation algorithms for satellite-derived leaf area index using the Data Assimilation Research Testbed (version Lanai)

... rithms can improve the LAI estimation. For boreal regions, there are two maxima for the RMSD in May and Septem- ber respectively, which is also the period with abrupt vari- ation for the LAI value. During the growing ... See full document

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