Sentences with phrase «maximum temperatures range»

The summer months, when maximum temperatures range from 15 to 20 °C (59 to 68 °F), are popular with tourists, but a growing trend in winter sports keeps tourism pulsing year - round.

Maximum temperatures range from 30 °C in summer to 21 °C in winter.

Not exact matches

These data range from 1979 to 2015, with a maximum temperature of 32 ° Celsius.

The maximum range of deformation (the biggest difference between morning and afternoon positions) occurred when temperature variations were their greatest — usually in spring and fall, not during the summer.

For each species, they estimated maximum growth rates, optimal growth temperatures, and the temperature ranges within which the species could grow.

Diurnal temperature range (DTR) decreased by 0.07 °C per decade averaged over 1950 to 2004, but had little change from 1979 to 2004, as both maximum and minimum temperatures rose at similar rates.

Temperatures in November would range from an average 20 °C minimum to 30 °C maximum.

Titan has a thin atmospheric layer of roughly constant temperature above the troposphere, followed by an extensive stratosphere ranging from 50 to 200 km (30 to 120 miles) in altitude, where temperatures steadily increase with altitude to a maximum of 160 to 180 K (− 172 to − 136 °F, − 113 to − 93 °C).

We customized a temperature range such that the lower temperatures approached a 60 - second ceiling (the maximum time period; all rats were removed after 60 seconds), and the highest temperature elicited a response in 10 - 15 seconds (thus, not uncomfortable immediately, but within a dynamic range that could be measured easily).

However, when the temperature was in the low 40s, the maximum estimated driving range was reported at 230 miles.

It uses high - contrast organic lightemitting diode (OLED) technology for maximum visibility and indicates various conditions such as fuel consumption, ambient temperature and cruising range.

In the case of the top - of - the - range engine, there are a number of special modifications to the production process to do justice to the increased output and the resulting higher temperatures in the combustion chamber, thereby guaranteeing maximum reliability of the drive system.

Maximum and minimum February temperatures range from 33 F to -47 F.

Temperatures range between 13 and 24 °C elsius (55 and 75 °F ahrenheit), the maximum rain falls between June and December.

Maximum temperatures during the wet season typically range from 24C to 38C (75F to 100 F), with January and February being the hottest months.

Abstract — New data acquisitions are used to examine recent global trends in maximum temperature, minimum temperature, and the diurnal temperature range (DTR).

The model variables that are evaluated against all sorts of observations and measurements range from solar radiation and precipitation rates, air and sea surface temperatures, cloud properties and distributions, winds, river runoff, ocean currents, ice cover, albedos, even the maximum soil depth reached by plant roots (seriously!).

The oven can simmer, bake, dehydrate, pasteurize water, and more, with typical temperatures inside the units ranging from 210º to 260º F, with a maximum of about 300º F.

The result is that temperatures in recent decades exceed the maximum proxy estimate (including uncertainty range) for the past 1,300 years.

A reconstruction of Northern Hemisphere temperature from stalagmites shows that while the uncertainty range (grey area) is significant, the temperature in the latter 20th Century exceeds the maximum estimate over the past 500 years (Smith 2006).

On a seasonal basis the ranges between the daily maximum, minimum and average are all listed and the lowest ratio is that the daily minimum temperature range over the year is 77,000 times greater than the temperature difference that would result from the proposed 30 % reduction in emissions.

eCast's web - based interface allows easy access to meaningful forecast ranges, timescales and visualizations for maximum and minimum temperatures, as well as the probability of precipitation, over the next 10 - days.

Since 1950, it has been found that the global diurnal temperature range (DTR), the difference between the minimum temperature (Tmin) and the maximum temperature (Tmax) of daily surface air temperature, has been temporally decreasing in several places all over the world.

Her glacial - interglacial range is a bit larger, for example the last glacial maximum (LGM, ~ 20 ky) is nearer -6 °C than -5 °C, and the temperatures prior to the «mid Pleistocene transition» (circa 1 My, some say 1.2 My) are rather different.

I guess there is a range of temperatures over which this magical equation is deemed to hold and its seems we are living at temperatures where this «must be» non-linear equation has a maximum value for lambda (must be because: -1000 + celcius isn't physically real).

The «decreasing trend» discussed in this paper refers to a decrease in the range between the maximum and minimum daily temperatures.

Paleo temperature ranges of that 11 degree range correspond to maximum CO2 concentrations of around 295 ppm at the top end.

The temperature plots show observed daily maximum and minimum temperatures, the 1981 — 2010 average maximum and minimum temperature range, and the record maximum and minimum range.

Maximum growth occurs when a range of conditions are optimum — temperature, fertilisation, moisture etc etc..

Here's the abstract: Analyses of maximum temperature data from 49 stations in Nepal for the period 1971 — 94 reveal warming trends after 1977 ranging from 0.068 to 0.128 C yr21 in most of the Middle Mountain and Himalayan regions, while the Siwalik and Terai (southern plains) regions show warming trends less than 0.038 C yr21.

In most cases, these range from about 2 to 4.5 C per doubled CO2 within the context of our current climate — with a most likely value between 2 and 3 C. On the other hand, chapter 9 describes attempts ranging far back into paleoclimatology to relate forcings to temperature change, sometimes directly (with all the attendant uncertainties), and more often by adjusting model parameters to determine the climate sensitivity ranges that allow the models to best simulate data from the past — e.g., the Last Glacial Maximum (LGM).

Take a look at Hansen 1993, scaling from radiation changes in last glacial epoch (plain orbital mechanics affecting irradiation), 3 ± 1 °C, Chylek 2007, differences between the Holocene and the last glacial maximum, 1.3 °C to 2.3 °C, and Bender et al 2010, looking at the response from Mount Pinatubo and the volcanic aerosols, with current temperature ranges, 1.7 to 4.1 °C.

We examine a range of climate extremes, comprising the 10th and 90th percentiles of daily maximum (TX) and minimum (TN) temperatures, the 90th percentile of daily precipitation (PR90), and the 27 core Climate Daily Extremes (CLIMDEX) indices.

The difference between daytime and nighttime temperatures is also known as the diurnal temperature range (DTR — the difference between minimum and maximum daily temperature).

New analyses of daily maximum and minimum land - surface temperatures for 1950 to 1993 continue to show that this measure of diurnal temperature range is decreasing very widely, although not everywhere.

Mean annual temperatures range from 40 to 55 °F (4 to 13 °C), with the maximum temperature reaching about 93 °F (34 °C) and minimum temperatures between 16 and − 27 °F (− 9 and − 33 °C).

Differences in the amount of maximum temperature increase ranges from 1.29 °C to 2.92 °C, but why?

The consequences for models» predictions of the future temperature can be seen in Figure 4, which shows that the mesoscale model's projections of mean maximum summertime temperatures over the eastern US for July 2085 soar into the 95 - 110 °F range, while the corresponding predictions for the GCM range between 75 - 95 °F.

The lunar temperature range is from 123 °C maximum to -153 °C minimum, a range of 276 °C.

There is also a decrease in diurnal temperature range (DTR) since the night - time temperature minima warm faster than the daytime maxima in many locations (e.g., Dai et al., 2001).

Mi Cro August 30, 2014 at 2:53 pm Clive, that's all fine and dandy, except those warming trends did not take place globally, they were regional trends.............................. We are finalising an analysis for Australia that shows of the claimed 1 deg C or so of warming since 1900, the maximum temperature change based on unadjusted data is half that or less, so 0.45 degrees for the century in the USA would fall neatly in the range we estimate for Australia.

By themselves instrumental readings can have lots of flaws which range from observer error to instrumental error to the basic problem that very often the maximum and minimum temperatures were not captured.

Diurnal Temperature Range (DTR) = the difference between a day's maximum and minimum air teTemperature Range (DTR) = the difference between a day's maximum and minimum air temperaturetemperature.)

This is also known as a decreasing diurnal temperature range (DTR — the difference between minimum and maximum daily temperature).

Using surface measurements of maximum and minimum temperatures from the Global Daily Climatological Network data set, we find evidence of a weekly cycle in diurnal temperature range (DTR) for many stations in the United States, Mexico, Japan, and China.

.2005 and PS2004), with temperatures within ± 1 standard error (SE) of a reconstruction «scoring» 10 %, and regions within the 5 to 95 % range «scoring» 5 % (the maximum 100 % is obtained only for temperatures that fall within ± 1 SE of all 10 reconstructions).

It shows the range of variation in US monthly averages, with the orange being the monthly average daily maximum temperature across the US, the dark blue showing the monthly average daily minimum temperature, and the green the monthly mean.

To make climate sensitivity small you've got to assume some combination of forcings that is high and temperature increase that is low (ie take the maximum for greenhouse gases, negligible aerosol forcing, maximum solar forcing and the bottom of the temperature range).

The median changes in temperature and precipitation for December, January and February (DJF) and June, July and August (JJA), averaged over the period 2070 — 2099, were calculated from the high - end and non-high-end projections together with the maximum range from each group of models.

Note that these are the US averages — the full range of daily maximums and minimums for the US as a whole would be wider and the full range of individual location temperatures would be wider still.