The simulated effects of changing monthly temperature and precipitation included a distinctive dieback of extant trees at most locations, with only partial recovery of biomass in areas of today's temperate deciduous forest.
You can use the IB Risk Navigator to
simulate the effects of changes in your portfolio.
Not exact matches
The Warming Meadow's radiators raise average soil temperatures by about three degrees Fahrenheit, decrease growing season soil moisture by up to twenty percent and advance the spring snowmelt date by up to a month in order to
simulate predicted
effects of climate
change.
When the researchers
simulated a second
effect of climate
change in addition to warming, namely drought, the results were even the opposite as expected: The soil animals ate less, and also the microorganisms living in the soil showed a decline in respiration — an indication that they also consumed less food.
Since trends in convective rainfall are not easily detected in daily rainfall records, or well -
simulated by global or regional climate models, the researchers created a new tool to assess the
effects of climate
change on rainfall patterns and trends in dryland areas.
The model enables to explore the
effects of climate
change on forestry ecosystems under
changed environmental conditions and to
simulate different management scenarios and compare them.
Thanks to the marked altitude steps
of the East African mountains — genuine open - air laboratories — IRD scientists and their Kenyan partners from ICIPE, KEFRI and the University
of Nairobi
simulated the
effects of climate
change on crops.
However, a new University
of Minnesota study with more than 1,000 young trees has found that plants also adjust — or acclimate — to a warmer climate and may release only one - fifth as much additional carbon dioxide than scientists previously believed, The study, published today in the journal Nature, is based on a five - year project, known as «B4Warmed,» that
simulated the
effects of climate
change on 10 boreal and temperate tree species growing in an open - air setting in 48 plots in two forests in northern Minnesota.
«By improving how we
simulate the biological pump in the ocean, we both improve the model and reveal this unexpected resilience, whereby global - scale
changes to the physical properties
of the ocean have a smaller
effect on the biological pump.
Brovkin, V., et al., 2006: Biogeophysical
effects of historical land cover
changes simulated by six Earth system models
of intermediate complexity.
- a lot
of focus was put on sound
effects in order to immerse players in the world
of Hyrule - the development team worked with Sound Racer, a studio specialized in sound
effects - this studio also worked on Xenoblade Chronicles X - they recorded more than 10 000 different sounds for the game - the team used a school bag to
simulate the sound
of rubbing leather - for the sound
of «normal» footsteps, they mixed various kinds
of sands - for the sounds
of equipment, they had to search for various materials and find ways to use them - they used an actual block
of ice to recreate the sound
of footsteps on ice - with the ice block, it always ended up melting, or getting cracks when the staff had to walk on it - Link's footsteps were made by a woman - depending on Link's actions and the equipment he's using / wearing, the recorded sounds were separated out individually - the volume is
changed as needed to make a particular sound stand out - check out sound
effect samples here
The two scientists, with colleagues from the UK, the U.S., the Netherlands and Czechoslovakia, report in Nature Climate
Change that they used mathematical models to
simulate the
effect of temperature rise as a response to ever - greater global emissions
of greenhouse gases into the atmosphere, from the combustion
of fossil fuels.
For example, many mechanistic models used to
simulate the ecological
effects of climate
change operate at spatial resolutions varying from a single plant to a few hectares.
«Fig. 1a shows an averaged IRIS cloud - cleared... and land / island areas have been masked out... Figure 1c shows the component
of the
simulated spectrum that includes only the
effect of trace - gas
changes between 1970 and 1997 (omitting..
Rather than questioning the primary role
of the atmospheric CO2, our modelling results allow us to put forward that the atmospheric CO2 is not the whole story and that, owing to the overwhelming
effect and interplay between the paleogeography, the water cycle and the seasonal response, the climate system may undergo subtle climatic
changes (as the 4 °C global warming
simulated here between the Aptian and the Maastrichtian runs).
To test how well a climate model predicts possible
changes in ocean circulation due to climate
change, GISS scientists have
simulated the
effects of a massive flood
of fresh water some 8000 years ago.
The
simulated change of GM in the last 30 yr has a spatial pattern that differs from that during the Medieval Warm Period, suggesting that global warming that arises from the increases
of greenhouse gases and the input solar forcing may have different
effects on the characteristics
of GM precipitation.
We find that the multi-model
simulated responses to the
effect of anthropogenic forcing or the
effect of anthropogenic and natural forcing combined are consistent with observed
changes.
Climate scientist Kevin Trenberth also notes that the
change in the estimated aerosol forcing is mainly associated with indirect aerosol
effects, but half
of GCMs don't include these indirect
effects, and those that do actually tend to
simulate less warming.
As for your V&V discussion, I don't see the relevance
of it in this talk, but in the context
of physical science
of climate
change we have overwhelming evidence
of model usefulness and verification (water vapor feedback,
simulating the Pinatubo eruption
effects, ocean heat content
changes, stratospheric cooling, arctic amplification, etc).
In order to separate out the
effects of greenhouse gases (GHG), these analyses typically regress time series
of many observational variables — including latitudinally and / or otherwise spatially distinguished surface temperatures — on model -
simulated changes arising not only from separate greenhouse gas and natural forcings but also from other separate non-GHG anthropogenic forcings.
Tubiello, F.N., and F. Ewert, 2002:
Simulating the
effects of elevated CO2 on crops: Approaches and applications for climate
change.
We find that the major
effects of clouds on radiation
change are linked to known physical processes that are quite consistently
simulated by models.
Biogeophysical
effects of historical land cover
changes simulated by six Earth system models
of intermediate complexity.
As the forcing and resulting temperature
changes are small, internal variability has a significant
effect on
simulated changes even when comparing 25 year means, with
changes varying in sign over some land areas and most
of the ocean.
Simulated radiative no - feedback
effects of measured actual CO2
change over the 61 years were calculated and found to be
of magnitude easily detectable by the empirical data and analytical methods used.