Sure enough, looking
at seasonal temperature anomalies we can see various curves like this:
-- Fermentation
at seasonal temperatures results in capsules that have a three - year shelf - life at room temperature.
I will also add this that looks
at seasonal temperatures on a more fine - grained decadal scale than the one you linked.
Not exact matches
The fare that appeals most during warm weather is fresh,
seasonal, and tastes best
at room
temperature.
Zara has a great military blazer
at the moment that's the perfect lightweight military jacket to combat the awkward
seasonal summer - into - fall
temperature change.
Meanwhile, permafrost observers the world over will take measurements in boreholes
at least 30 meters (100 feet) deep — the depth where
temperatures do not fluctuate during
seasonal cycles — though some will stretch much deeper.
The team used real - time
seasonal rainfall,
temperature and El Niño forecasts, issued
at the start of the year, combined with data from active surveillance studies, in a probabilistic model of dengue epidemics to produce robust dengue risk estimates for the entire year.
The researchers also looked
at deviations of daily
temperatures from
seasonal averages in trying to determine the effect of anomalies on crime rates.
The data showed that the region experienced minimal
seasonal variation in
temperature and rainfall; in other words,
at most a very weak monsoon.
At the moment the company is working with NASA to develop technology that would predict how small - scale,
seasonal shifts in
temperature as well as large - scale climate change influence the presence of bacteria in the soil, air and water around crops.
By looking
at variables such as day and night
temperatures and
seasonal rainfall and vegetation types, for instance, researchers can identify the ecological niches best suited to certain insects.
After this process was used by the researchers to determine new normal conditions for global average
temperatures, it was used again to examine record hot
seasonal temperatures at a regional level.
At local scales and over shorter periods, annual streamflow responds to
seasonal changes in climate variables (e.g.,
temperature, precipitation) and related processes such as evapotranspiration.
Sadly the 50 - 60 degree weather we have been experiencing in central Ohio for the past week or so has been replaced by the
seasonal arctic
temperatures one would expect
at this time Keep Reading
But below -
seasonal temperatures combined with too many timid motorists crawling along
at a snail's pace
at the first sign of a snowflake have had a negative effect on my psyche.
Changes in the outdoor
temperature at every season will require you to make
seasonal adjustments to the
temperature and humidity controls for your reptile or amphibian.
[Response: Hansen et al. look
at seasonal anomalies, especially those for the average
temperature of June - July - August.
In temperate climates strong
seasonal waterborne infections like the norovirus, rotavirus, salmonella, campylobacter and — differing from the usual dogma — influenza are mainly triggered by drinking water, dependent on the water's
temperature (in Germany it is
at a minimum in February and March and
at a maximum in August).
In temperate climates the lethal H5N1 virus will be transferred to humans via cold drinking water, as with the birds in February and March 2006, strong
seasonal at the time when drinking water has its
temperature minimum.
The reason is that if an ice sheet is
at a
temperature of say ~ 20 oC where it never undergoes a
seasonal melt, then even a very large
temperature increase (say 10 oC) isn't going to make it melt either!
Re 9 wili — I know of a paper suggesting, as I recall, that enhanced «backradiation» (downward radiation reaching the surface emitted by the air / clouds) contributed more to Arctic amplification specifically in the cold part of the year (just to be clear, backradiation should generally increase with any warming (aside from greenhouse feedbacks) and more so with a warming due to an increase in the greenhouse effect (including feedbacks like water vapor and, if positive, clouds, though regional changes in water vapor and clouds can go against the global trend); otherwise it was always my understanding that the albedo feedback was key (while sea ice decreases so far have been more a summer phenomenon (when it would be warmer to begin with), the heat capacity of the sea prevents much
temperature response, but there is a greater build up of heat from the albedo feedback, and this is released in the cold part of the year when ice forms later or would have formed or would have been thicker; the
seasonal effect of reduced winter snow cover decreasing
at those latitudes which still recieve sunlight in the winter would not be so delayed).
There can / will be local and regional, latitudinal, diurnal and
seasonal, and internal variability - related deviations to the pattern (in
temperature and in optical properties (LW and SW) from components (water vapor, clouds, snow, etc.) that vary with weather and climate), but the global average effect is
at least somewhat constrained by the global average vertical distribution of solar heating, which requires the equilibrium net convective + LW fluxes, in the global average, to be sizable and upward
at all levels from the surface to TOA, thus tending to limit the extent and magnitude of inversions.)
Additionally, the publication aims to highlight the full range climate - related health issues and risks (i.e. nutrition, NCDs, air pollution, allergens, infectious diseases, water and sanitation, extreme
temperatures and weather, etc.) where health decision - making can benefit from climate and weather knowledge
at historic, immediate,
seasonal, or long - term time scales.
Moreover, the
seasonal, regional, and atmospheric patterns of rising
temperatures — greater warming in winters than summers, greater warming
at high latitudes than near the equator, and a cooling in the stratosphere while the lower atmosphere is warmer — jibe with what computer models predict should happen with greenhouse heating.
(There may be some kinds of trend in the model, for example
seasonal trends, but they are all «overruled»
at every measured
temperature.).
ECHAM3
at T42 improved the
seasonal cycle of surface
temperature in seven regions, compared to the driving AOGCM, but overall surface
temperature was too high (by 2 to 5ºC).
The three different ozone databases yield changes in tropical lower stratospheric
temperatures that differ by more than a factor of two
at 70 mbar, although all have qualitatively similar
seasonal cycles.
Thus the first year (s)
temperature change is the most responsible for the first year (s) change in CO2 increase, but as the
temperature influence is limited in time (a different, but constant
temperature again gives a constant
seasonal cycle, but
at a different level), the next years that will not give a change in increase speed anymore.
If one looks
at the ocean / water
temperatures http://weather.unisys.com/surface/sst.html there are enormous differences between the tropics, temperate and north, and enormous
seasonal variations during the year which will affect CO2 absorption and emission, and there is a lot of biological activity in seas and waters that also are involved.
Have a look
at the
seasonal changes
at Mauna Loa: The influence of
temperature is clear: warmer in this case means more CO2 eaten away by vegetation and reverse when
temperatures in the NH drop.
See http://data.giss.nasa.gov/gistemp/graphs/ (the
seasonal mean
temperature change graph
at the bottom) to see what I mean.
Specifically, the cloud cover is multiplied by the factor 1 + c T, where T, computed every time step, is the deviation of the global mean surface air
temperature from the long - term mean in the model control run
at the same point in the
seasonal cycle and c is an empirical constant.
Boreholes do not retain any information relating to surface
temperature at any depth beyond the
seasonal influence of the Sun.
They suggest that management strategies currently employed in marginal production areas that moderate
temperatures and offset mismatches between the needs of the plant
at various growth stages and
seasonal weather conditions may be useful adaptation strategies.
Climate scientists hate it when people show real
temperature because it is impossible to see much warming when you look
at the
seasonal changes in the actual
temperature.
The global warming signal itself is a multidecadal feature of the climate, but just like the
seasonal example above, it has been possible
at times to take one period of one
temperature record - surface air
temperatures in most cases - and do a «January - February» job with it, thereby making the claim that
temperatures are flatlining or even cooling.
Have a look
at Cohen et al. (2012) Asymmetric
seasonal temperature trends.
One explanation for the
seasonal offset is that the large summertime snow / ice change alters ground
temperatures, and these ground
temperature changes are felt more
at ground - level during winter when the surface atmospheric layer is most stable.
Season or specific months: (A)
Seasonal temperatures are of particular interest because Polar Regions
at high latitudes are an outstanding example of the considerable impact and influence of the sun decreases in wintertime as far down as the North - and Baltic Sea (both above 50 ° North).
The impacts of the marked
seasonal variability of factors such as net radiation and / or
temperature at high latitude sites are of far more importance for tree growth than the small
seasonal variation in CO2 (a well - mixed gas).
A = maximum
temperature measurement,
at Airport B = minimum
temperature measurement,
at Airport UHI * - a = slowly varying
seasonal value of the UHI,
at Airport UHI * - s = slowly varying
seasonal value of the UHI, in Suburbia Tmax - a = «true» maximum
temperature,
at Airport Tmax - s = «true» maximum
temperature, in Suburbia
New record highs have been set for monthly and
seasonal average
temperatures across Australia
at 12 times the rate of new record lows.
Positive forcing
at seasonal to inter-annual scales leads to an average global surface
temperature drop from La Nina influence but recharging of OHC (longer term gain), while reduced forcing allows El Nino conditions and temporary peaks in global average
temperature, and OHC reduction (longer term loss).
As shown in Figure 3 above, light dry soils experience greater
seasonal temperature swings
at a given depth than wet soils.
The following are more of interest: — «Winter Sampling of Shallow Firn Air
at the South Pole to Understand Processes Affecting Firn Atmospheric Histories and Ice Core Gas Records» by Severinghaus (2000), — «Thermal fractionation of air in polar firn by
seasonal temperature gradients» by Severinghaus, Grachev & Battle (2001), — «Severinghaus et al. «Fractionation of gases in polar ice during bubble close - off: New constraints from firn air Ne, Kr and Xe observations» by Severinghaus & Battle (2006), but all follow the same line of reasoning.
These unique fingerprints are easier to see by probing beyond a single number (such as the average
temperature of Earth's surface), and looking instead
at the geographical and
seasonal patterns of climate change.
Scientists also factored long - term, climate change trends into the three - month
seasonal outlook by looking
at the last 10 to 15 years of
temperature and precipitation across the country.
Scientists use permafrost
temperature, measured
at a depth where
seasonal variations cease to occur, as an indicator of long - term change and to represent the mean annual ground
temperature.
PCIC has made
seasonal maps of average
temperature and total precipitation departures from the 30 - year climatology
at observational weather stations in BC, for all months from 1972 onward.
Therefore, as in our time - series analyses of annual proportions of male births and stillbirths, we found no support for the hypothesis that
seasonal variation in ambient
temperature at the time of conception is related to the proportion of male births in New Zealand.