Not exact matches
The climate is steady and hot,
with an average
yearly temperature of 28º C (82º F).
Even
with a long - term background trend of rising
temperatures, other climate factors contribute to
yearly ups and downs.
These
yearly rings change
with temperature and rainfall, so they could read past weather by calibrating ring widths of living trees
with instrumental data from 1959 - 2009, then comparing these
with the innards of much older trees.
The area enjoys comfortable
temperatures all year round and can expect a
yearly average of 300 sunny days
with fresh Atlantic breezes taming the heat of high summer.
With a tropical and warm climate, average
yearly temperatures range from 28 °C (82 °F) to nearly 31 °C (88 °F).
Climate: One of the nicest things about visiting Belize it is sub-tropical
with an average
yearly temperature of 84 ° F (29 °C), it's always warm, yet comfortable.
Step off the plane and feel the warm embrace of Kauai
with average
yearly temperatures ranging between 84 and 69 degrees.
Water
temperature varies little
with a
yearly average of 24oC (76 F).
At approximately 1400 meters above sea level, Monteverde is cold,
with an average
yearly temperature of 18 degrees Celsius / 64.4 degrees Fahrenheit
The southernmost town of Europe,
with an average
temperature of 20,1 °C, few rainfalls (average 440 mm of rain
yearly) and a
temperature that rarely dropping below 12 °C.
«The 2 \ sigma uncertainty in the global mean anomaly on a
yearly basis are (
with the current network of stations) is around 0.1 ºC in contrast that to the estimated uncertainty in the absolute
temperature of about 0.5 ºC (Jones et al, 1999).»
The 2 uncertainty in the global mean anomaly on a
yearly basis are (
with the current network of stations) is around 0.1 ºC in contrast that to the estimated uncertainty in the absolute
temperature of about 0.5 ºC (Jones et al, 1999).
It now spends the vast majority of the money it does have fighting
yearly blazes,
with little left over to prepare for warming
temperatures.
However, CO2 does not rise and fall
with the
temperature on an hourly, daily or even
yearly basis.
It is instructive to compare these numbers
with those characteristic of a set of the years during 1979 — 2012
with no or only one major regional extreme event (in terms of land surface
temperature and land precipitation anomalies) in the NH midlatitudes, from late April / early May to late September / early October, as reported
yearly since 1993 in the World Meteorological Organization statements on the status of the global climate (see also ref.
It reminds of the efforts or lack thereof of the dendros in using pre-selected samples and then regressing
with first TRs for the
yearly temperature and than a combination of TRs and MXDs for selected months of the year «$» all without clearly delineating the basic biological processes involved.
As an example, my long - term prediction for the
temperature of Colorado Springs is that it will vary within the range of -40 C to 40C,
with daily and
yearly oscillatory components.
Moreover the recent decline of the
yearly increments d (CO2) / dt acknowledged by Francey et al (2013)(figure 17 - F) and even by James Hansen who say that the Chinese coal emissions have been immensely beneficial to the plants that are now bigger grow faster and eat more CO2 due to the fertilisation of the air (references in note 19) cast some doubts on those compartment models
with many adjustable parameters, models proved to be blatantly wrong by observations as said very politely by Wang et al.: (Xuhui Wang et al: A two-fold increase of carbon cycle sensitivity to tropical
temperature variations, Nature, 2014) «Thus, the problems present models have in reproducing the observed response of the carbon cycle to climate variability on interannual timescales may call into question their ability to predict the future evolution of the carbon cycle and its feedbacks to climate»
Yearly and monthly
temperature records have been breaking regularly,
with many of the records being broken by the biggest margins ever seen.
The TAR discussed various attempts to use proxy data to reconstruct changes in the average
temperature of the NH for the period after AD 1000, but focused on three reconstructions (included in Figure 6.10), all
with yearly resolution.