This information
increases global climate simulation accuracy through better representation of deep ocean heat and carbon fluxes.
Not exact matches
Global simulations conducted by the team found that microbial responses to enhanced root activity under rising CO2, while depending on plant species, climate and soil mineralogy, led to a loss of global soil carbon stocks that counteracted the additional carbon storage resulting from increased plant growth in many regions of the
Global simulations conducted by the team found that microbial responses to enhanced root activity under rising CO2, while depending on plant species,
climate and soil mineralogy, led to a loss of
global soil carbon stocks that counteracted the additional carbon storage resulting from increased plant growth in many regions of the
global soil carbon stocks that counteracted the additional carbon storage resulting from
increased plant growth in many regions of the world.
Overall, ecosystem - driven changes in chemistry induced
climate feedbacks that
increased global mean annual land surface temperatures by 1.4 and 2.7 K for the 2 × and 4 × CO2 Eocene
simulations, respectively, and 2.2 K for the Cretaceous (Fig. 3 E and F).
In a recent paper by Bengtsson & Hodges (2006),
simulations with the ECHAM5
Global Climate Model (GCM) were analysed, but they found no
increase in the number of mid-latitude storms world - wide.
# 5:
Global climate model
simulations that include greenhouse gases indicate that the magnitude of warming that would be expected from greenhouse gas
increases is at least as large as the observed warming.
««
Climate model
simulations that consider only natural solar variability and volcanic aerosols since 1750 — omitting observed
increases in greenhouse gases — are able to fit the observations of
global temperatures only up until about 1950.»
However, there is not compelling evidence that anthropogenic CO2 was sufficient to influence Earth's temperatures prior to 1950, i.e. «
Climate model
simulations that consider only natural solar variability and volcanic aerosols since 1750 — omitting observed
increases in greenhouse gases — are able to fit the observations of
global temperatures only up until about 1950.»
Trends in
climate variables and their interrelationships over China are examined using a combination of observations and
global climate model
simulations to elucidate the mechanism for producing an observed 1 °C
increase in surface temperature despite a significant decrease in surface insolation from 1950 to 2000.
(07/08/2013) Warmer ocean temperatures will
increase the frequency and intensity of tropical cyclones, typhoons and hurricanes in «most locations» this century, concludes a new study based on
simulations using six
global climate models.
For example,
global mean runoff has been simulated to
increase by 5 % -17 % due to
climate change alone in an ensemble of 143 2 * CO2 GCM
simulations (Betts et al., 2006).
Coupled
simulations, using six different models to determine the ocean biological response to
climate warming between the beginning of the industrial revolution and 2050 (Sarmiento et al., 2004), showed
global increases in primary production of 0.7 to 8.1 %, but with large regional differences, which are described in Chapter 4.
Baseline (i.e., mean 1971 — 1999)
global varies between 461 Pg C and 998 Pg C, and
increases with ΔMLT for all vegetation models under all 110
climate and CO2
increase scenarios (Fig. 1)(see Materials and Methods and SI Text for details of
simulations).
The
simulations also produce an average
increase of 2.0 °C in twenty - first century
global temperature, demonstrating that recent observational trends are not sufficient to discount predictions of substantial
climate change and its significant and widespread impacts.
The new position statement is equivocal, beginning with the observation that «the AAPG membership is divided on the degree of influence that anthropogenic CO2 has on recent and potential
global temperature
increases», and going on to say «Certain
climate simulation models predict that the warming trend will continue, as reported through NAS, AGU, AAAS, and AMS.
The radative forcing (left) and
global mean temperature response (right) using a simple GCM emulator, for the historical CO2 forcing (red) and for the linearly
increasing forcing consistent with the
simulations used to define the transient
climate response (blue), for 3 different ramp - up time scales, the 70 year time scale (solid blue) corresponding to the standard definition.