L5 Flashcards

1
Q

Land-surface models/ vegetation models

A
  • Computer based model
    • Used to simulate land processes
    • Numerical models that solves the coupled fluxes of water, energy and carbon between the land-surface and atmosphere, within a context of direct and indirect human forcings and ecological dynamics
    • They are also known as terrestrial carbon models, dynamic global vegetation model (DGVM)
    • Names come from configurations they have
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2
Q

Land surface models work for simplified configurations eg for:

A
  • Meteorology
  • Soil ecology
  • Vegetation dynamics
  • Hydrology
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3
Q

Land surface models also work for full-complexity configurations eg:

A
  • These resolve many cycles/ patterns etc
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4
Q

How can we use land surface models?

A

independently or within an Earth system model

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5
Q

We can use land-surface models independently or within an Earth System Model

A
  • An earth system model is a set of models that can be run independently or together to simulate the Earth global climate
    • Land model is an important component of Earth System models
    • Land- surface models can involve complex code all centred by the coupler which connects eg land ice to ocean
    • These models are ran in high performance computing systems (HPC)
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6
Q

Examples of terrestrial feedbacks within the Earth system (components of land-surface model)

A
  • Snow cover and climate
    • Soil moisture- evapotranspiration- precipitation
    • Land use and land cover change
    • Carbon cycle
    • Reactive nitrogen
    • Chemistry-climate (BVOCs, O3, CH4, aerosols)
    • Biomass burning (fires)
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7
Q

Land is a critical … of CO2 emissions

A

Sink

  • Trees involved in the model produce CO2 etc
  • These models can tell us implications of future emissions etc
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8
Q

Many land-surface models available

A
  • Often ran in conjunction with one another
    • 16 land-models participated in the 2022 carbon budget
    • They vary in what they feature eg fires vs no fires
    • Often have different configurations but are made by the same companies
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9
Q

How do land-surface models work in the global carbon budget?

A
  • Take an average from the land models results
    • Provide certain elements towards the carbon budget others eg gas reserve etc which are not in land-surface models
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10
Q

How are land models interdisciplinary?

A
  • Started off very simple then added more ecosystem functions to the land model
    • Evolved from land as a lower boundary to the atmosphere to land as an integral component of the Earth system
  • Developed along with computer capability and research questions
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11
Q

What is the role of a land model in an Earth system model?

A

Land-atmosphere exchanges
- Energy, water vapour, CO2, dust, trace gases

Land surface states
- Soil moisture, soil temperature, canopy temperature, snow water equivalent, C and N stocks

Land surface characteristics
- Soil texture, surface roughness, albedo, emissivity, vegetation type, LAI index
  • When using a land model all these fluxes are passed from land to atmosphere whilst conserving each other
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12
Q

What are the main components of a land model?

A
  • Surface energy fluxes
    • Hydrology
    • Biogeochemical cycles

The land surface model solves surface energy balance , surface water balance and carbon balance equations at each model timestep

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13
Q

surface energy balance inputs or forcings

A
  • Direct solar and Incoming long wave radiation
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14
Q

surface energy balance outgoings

A

Response fluxes

- Reflected solar

- Outgoing longwave
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15
Q

The land surface affects the energy balance through what three properties?

A

Albedo
Surface Roughness
Evapotranspiration

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16
Q

Land models can look at the … effect

A

temperature effect eg converting forest to cropland

17
Q

albedo directly affects…

A

net radiation

trees are darker than grasses and have lower albedo

18
Q

surface roughness affects…

A

sensible and latent heat fluxes

trees are tall and aerodynamically rough

grasses are warmer and drier

19
Q

latent heat flux…

A

evaporatively cools

trees transpire more water than grasses

20
Q

influence of deforestation on climate - if we took all forest and converted it to grassland (on the three properties)

A
  • Albedo only shows a decrease in temperature
    • Trees absorb more radiation as they are darker
    • Evapotranspiration shows a warming effect
  • Forests evapotranspire more than grass and cool

Surface roughness shows a warming effect

21
Q

net response (annual mean)

A
  • Deforestation both increases and decreases temperature depending on location
  • Deforestation cools higher latitudes but warms tropical latitudes
22
Q

surface water balance

A
  • Also needs to resolve other water balances such as snow and soil water
  • Precipitation comes in
  • Various evaporation and runoff methods
    • Models also needs to resolve change in soil moisture over time
23
Q

surface carbon balance

A
  • Model computes net ecosystem exchange (NEE)
    • Depends on GPP
    • GPP = gross primary productivity (photosynthesis)
    • Losses out of the system from respiration, carbon lost through fire and land use change
  • Resolves plant and soil carbon pools
24
Q

land use change … total C storage

A

decreases

- When cropland is replaced

- Forest stores more carbon than grasslands
25
Q

Land modelling challenges: Land surface heterogeneity

A
  • Models are ran at 100 x 100km resolution (low)
  • Take into account heterogeneity by the process of subgrid tiling
26
Q

Subgrid tilling

A
  • Grid cell is divided by land unit
  • Land units involve eg vegetated, lake, urban, glacier, crop
  • Soil column is then placed into natural land units where soil occurs
  • Patches are then defined in vegetated column into plant functional types
27
Q

Urban land unit

A
  • Features configurations eg roofs, sun walls, shade walls,
28
Q

Glacier

A
  • Elevation classes
29
Q

Crops

A

Unrrig, irrig

30
Q

How does land unit work?

A
  • Each grid cell has a percentage of the type of land unit
  • We don’t know eg where lakes will be, but we know the percentage of it lakes shall make up
  • Information comes from satellite data
  • Resolve energy etc for each land unit and provides an output per grid cell weighted depending on land unit percentage
  • Land surface models are parameter heavy
31
Q

Where do parametrisations in land models come from?

A
  1. Laboratory understanding
    • Of plant physiological processes
    1. Empirical relationships
      - From as large a sample of the real world as possible, from field and satellite observations
    2. Optimality theory
      - Plants are rational actors, on average
32
Q

Sources of uncertainty in land-surface modelling

A
  1. Forcing (scenario) uncertainty, GHG emissions scenarios, land use etc
    1. Response (model) uncertainty from parameterisations, resolution etc
      - Using multiple models corrects for this
    2. Internal (natural or unforced) variability; initial value problems
      - Running several temperatures eg air temperature
      - Several experiments
33
Q

Paths to reducing model uncertainty

A

model intercomparisons
model intracomparison
model benchmarking
model data-fusion
comparison to real- world manipulative experimens
model hierarchy

34
Q

conclusions

A
  • Land models enable scientists and policymakers to better understand and manage the Earth’s natural resources, and to address some of the most pressing environmental challenges for our time
    • Land-surface models are a starting point for the science, but not the science itself
    • Land surface models are very complex and multidisciplinary, however are easy to run, but hard to interpret