In addition,
changes in mean annual temperature had no effect on the proportion of male stillbirths.
Even seemingly «straightforward» applications like the assessment of the impact of
changes in the mean annual cycle of temperature on shifting butterfly populations did find more climate variables than just temperature to be of importance (see e.g. WallisDeVries et al, 2011; http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3172409/), and this generally applies to many sectors and applications.
Interpolated surfaces showing
the change in mean annual temperature across Alaska for three different time series: 1949 − 2009, 1949 − 1976, and 1977 − 2009.
Not exact matches
With some smart planning and a positive attitude, this
annual period of
change can become a special marker of growth and
meaning in your family's life.
Tracking shifts
in the distribution of these
annual histograms provides a new integrated measure of energy balance components and land - cover
change, and a different
means to monitor biospheric
change.
These events took place within millennia — fairly quickly, on a climatic time scale — and resulted
in changes of up to 10 degrees Celsius
in mean annual temperatures.
«Looking at
changes in the number of dry days per year is a new way of understanding how climate
change will affect us that goes beyond just
annual or seasonal
mean precipitation
changes, and allows us to better adapt to and mitigate the impacts of local hydrological
changes,» said Polade, a postdoctoral researcher who works with Scripps climate scientists Dan Cayan, David Pierce, Alexander Gershunov, and Michael Dettinger, who are co-authors of the study.
«
In particular the United States, southern South America, southern Africa, central and southern Europe, Southeast Asia and southern Australia are vulnerable regions, because declines in mean annual streamflow are projected combined with strong increases in water temperature under changing climat
In particular the United States, southern South America, southern Africa, central and southern Europe, Southeast Asia and southern Australia are vulnerable regions, because declines
in mean annual streamflow are projected combined with strong increases in water temperature under changing climat
in mean annual streamflow are projected combined with strong increases
in water temperature under changing climat
in water temperature under
changing climate.
For the
change in annual mean surface air temperature
in the various cases, the model experiments show the familiar pattern documented
in the SAR with a maximum warming
in the high latitudes of the Northern Hemisphere and a minimum
in the Southern Ocean (due to ocean heat uptake)(2)
has decreased
in winter, but no significant
change in annual mean precipitation potentially because of very slight increases
in spring and fall precipitation; precipitation is projected to increase across Montana, primarily
in spring; slight decrease
in summer precipitation; variability of precipitation year - to - year projected to increase
(Top left) Global
annual mean radiative influences (W m — 2) of LGM climate
change agents, generally feedbacks
in glacial - interglacial cycles, but also specified
in most Atmosphere - Ocean General Circulation Model (AOGCM) simulations for the LGM.
b, d, f and h show the
change in frequency of the number of years with anomalous
mean annual weather conditions (> 1σ above historical
mean) from 1996 to 2013 compared with the number of anomalies observed from 1979 to 1996.
To contribute to an understanding of the underlying causes of these
changes we compile various environmental records (and model - based interpretations of some of them)
in order to calculate the direct effect of various processes on Earth's radiative budget and, thus, on global
annual mean surface temperature over the last 800,000 years.
Abstract:» The sensitivity of global climate with respect to forcing is generally described
in terms of the global climate feedback — the global radiative response per degree of global
annual mean surface temperature
change.
Statewide precipitation has decreased
in winter (0.14 inches / decade -LSB--0.36 cm / decade]-RRB- since 1950, but no significant
change has occurred
in annual mean precipitation, probably because of very slight increases
in spring and fall precipitation.
So, to enter the teaching profession later
in life
means about four years of full - time study, a
change in annual income and possibly one to three years of casual work.
Some said the additional time
meant a better chance of compromise
in North Carolina's
annual tilting match between traditional schools and charter supporters, who claim that publicly - funded charters are being short -
changed by their traditional school counterparts.
Coming off its best half - year since 2008, the U.K. car build was down 11.2 % year - on - year
in July as
changes to holiday patterns
meant the traditional
annual shutdown started earlier at some plants.
Sure,
annual renters insurance reviews might
mean you should increase or
change your coverage to reflect
changes in your lifestyle.
Usually, having a subprime credit score
means you have to settle for less than stellar options or high
annual fees, but the Discover it ® Secured Card — No Annual Fee has changed up the secured credit card scene in a majo
annual fees, but the Discover it ® Secured Card — No
Annual Fee has changed up the secured credit card scene in a majo
Annual Fee has
changed up the secured credit card scene
in a major way.
A half - life of 1.0 typically
means roughly 100 %
annual portfolio turnover; a half - life of 10.0
means only about one - tenth of the portfolio turns over
in any given year.8 Strategies and factors with longer half - lives, such as small cap and profitability, are likely to have portfolios that
change slowly from one year to the next, making it much easier to tease out the structural alpha.
In the first entry I discussed product
changes,
meaning my plans to
change either from
annual - fee to no -
annual - fee versions (like the Barclaycard Arrival World MasterCard), or to more lucrative versions (Citi Dividend Platinum Select), of the cards I currently carry — while keeping my credit limits and age of accounts intact.
The warming trends
in looking at numerous 100 year temperature plots from northern and high elevation climate stations... i.e. warming trends
in annual mean and minimum temperature averages, winter monthly
means and minimums and especially winter minimum temperatures and dewpoints... indicate climate warming that is being driven by the accumulation of greenhouse gases
in the atmosphere — no visible effects from other things like
changes in solar radiation or the levels of cosmic rays.
... Polar amplification explains
in part why Greenland Ice Sheet and the West Antarctic Ice Sheet appear to be highly sensitive to relatively small increases
in CO2 concentration and global
mean temperature... Polar amplification occurs if the magnitude of zonally averaged surface temperature
change at high latitudes exceeds the globally averaged temperature
change,
in response to climate forcings and on time scales greater than the
annual cycle.
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).
Abstract:» The sensitivity of global climate with respect to forcing is generally described
in terms of the global climate feedback — the global radiative response per degree of global
annual mean surface temperature
change.
The song took on new
meaning for me
in 2003, when I accompanied a team of climate and ocean researchers on their
annual expedition aimed at studying
changes in the Arctic Ocean beneath the shifting sea ice just a few dozen miles from the North Pole.
The 4 W / m2 solar constant
change you quote (which is at the high end), is around 0.7 W / m2
in global
annual mean radiaitve forcing, compared to 2.4 W / m2 from CO2 + CH4 + N2O — still a small number.
They discussed the effect of variables being non-iid on the extreme value analysis, and after taking that into account, propose that
changes in extreme precipitation are likely to be larger than the corresponding
changes in annual mean precipitation under a global warming.
The key is that the tropical Pacific is actually very well sampled (through the TOGA - COARE array) and the patterns you see
in the
annual means change slowly enough for the heat content anomalies to be well characterised.
Basically, mathematicians have devised a
means by which they can take oscillatory data and,
in essence, subtract out known cycles
in order to observe how the data is
changing independent of these known
annual, solar, and paleoclimatic cycles.
The global map of the A1B 2080 to 2099
change in annual mean precipitation is shown
in Figure 10.12, along with other hydrological quantities from the multi-model ensemble.
«
In considering the question of human activity and climate change it is essential to distinguish between global warming, which is a progressive increase in the annual mean global temperature, and human - activity - induced greenhouse warming, as may, for example, be caused by the release of greenhouse gases into the atmosphere as a result of fossil fuel combustion or deforestation.&raqu
In considering the question of human activity and climate
change it is essential to distinguish between global warming, which is a progressive increase
in the annual mean global temperature, and human - activity - induced greenhouse warming, as may, for example, be caused by the release of greenhouse gases into the atmosphere as a result of fossil fuel combustion or deforestation.&raqu
in the
annual mean global temperature, and human - activity - induced greenhouse warming, as may, for example, be caused by the release of greenhouse gases into the atmosphere as a result of fossil fuel combustion or deforestation.»
Seasonal
changes in insolation are much larger than
annual mean changes and can reach 60 W m — 2 (Box TS.6, Figure 1).
Figure B shows the scenario for the
change in annual mean temperature per 1 C global warming using this method for 248 meteorological stations.
These cycles
change the amount of solar radiation received at each latitude
in each season (but hardly affect the global
annual mean), and they can be calculated with astronomical precision.
By comparing modelled and observed
changes in such indices, which include the global
mean surface temperature, the land - ocean temperature contrast, the temperature contrast between the NH and SH, the
mean magnitude of the
annual cycle
in temperature over land and the
mean meridional temperature gradient
in the NH mid-latitudes, Braganza et al. (2004) estimate that anthropogenic forcing accounts for almost all of the warming observed between 1946 and 1995 whereas warming between 1896 and 1945 is explained by a combination of anthropogenic and natural forcing and internal variability.
Changes in obliquity modulate seasonal contrasts as well as annual mean insolation changes with opposite effects at low vs. high latitudes (and therefore no effect on global average insolation)-LCB- 6.4
Changes in obliquity modulate seasonal contrasts as well as
annual mean insolation
changes with opposite effects at low vs. high latitudes (and therefore no effect on global average insolation)-LCB- 6.4
changes with opposite effects at low vs. high latitudes (and therefore no effect on global average insolation)-LCB- 6.4 -RCB-.
«With the U.S. hemp industry valued at an estimated $ 500 million
in annual retail sales and growing, a
change in federal policy to once again allow hemp farming would
mean instant job creation, among many other economic and environmental benefits,» adds Steenstra.
Models disagree on
annual mean precipitation
changes in the NA monsoon region.
Here we construct a database of worldwide RS observations matched with high - resolution historical climate data and find a previously unknown temporal trend
in the RS record after accounting for
mean annual climate, leaf area, nitrogen deposition and
changes in CO2 measurement technique.
«With the U.S. hemp industry valued at over $ 400 million
in annual retail sales and growing, a
change in federal policy to once again allow hemp farming would
mean instant job creation, among many other economic and environmental benefits,» adds Steenstra.
equilibrium climate sensitivity refers to the equilibrium
change in the
annual mean global surface temperature following a doubling of the atmospheric equivalent carbon dioxide concentration.
«With the U.S. hemp industry estimated at over $ 500 million
in annual retail sales and growing, a
change in federal law to allow colleges and universities to grow hemp for research
means that we will finally begin to regain the knowledge that unfortunately has been lost over the past fifty years,» says Vote Hemp President Eric Steenstra.
On a (2011) Climate Etc. post Pondering the Arctic Ocean, I interpreted the record
in the context of a (qualitative)
change point analysis, defined by
changes in trend,
mean value, amplitude of the
annual cycle, and interannual variability.It looks like 2013 was another
change point year, characterized by low amplitude seasonal cycle.
Figure 3, from Hansen & Lebedeff 1987 (apologies for the poor quality, this is an older paper) plots the correlation coefficients versus separation for the
annual mean temperature
changes between randomly selected pairs of stations with at least 50 common years
in their records.
I do not believe that global
mean annual temperatures have simply cooled progressively over thousands of years as Mike appears to and I contend that that there is strong evidence for major
changes in climate over the Holocene (not Milankovich) that require explanation
Instead of
changes in monthly values of Temp and precip (and cloud cover)
changes in ANNUAL mean temperature were used to force LPJ.
All these stations indicate the same pattern of
changes in annual mean temperature: a warm 1930s, a cooling until around 1970, and thereafter a warming, although the temperature remains slightly below the level of the late 1930s.
Background map: Ensemble
mean change of
annual runoff,
in percent, between present (1981 to 2000) and 2081 to 2100 for the SRES A1B emissions scenario (after Nohara et al., 2006).