Sentences with phrase «temperature precipitation distribution»

Position on a Continent Temperature Precipitation Distribution of Climate Regions - Due to water's better ability to hold heat longer, areas around coastlines tend to have warmer climates than areas that are further away from water.

Latitude Temperature Precipitation Distribution of Climate Regions Latitude has the greatest impact on climate since it determines the amount of sunlight an area receives.

Not exact matches

The mean width of a ring in any one tree is a function of many variables, including the tree species, tree age, availability of stored food within the tree and of important nutrients in the soil, and a whole complex of climatic factors (sunshine, precipitation, temperature, wind speed, humidity, and their distribution througnout the year).

As Bradley points out, tree growth, and hence the width and density of tree rings, depends on many factors, including the tree species and age, the availability of stored food in the tree and nutrients in the soil, the full range of climatic variables (sunshine, precipitation, temperature, wind speed, humidity); and their distribution throughout the year.

tree growth, and hence the width and density of tree rings, depends on many factors, including the tree species and age, the availability of stored food in the tree and nutrients in the soil, the full range of climatic variables (sunshine, precipitation, temperature, wind speed, humidity); and their distribution throughout the year.»

Climate zones are based on natural vegetation groupings, precipitation patterns, and temperature distribution.

Greater numbers of plant species in ruderal based environments were found in equatorial areas where the level of water (represented by mean annual precipitation) related variables are high, whereas competitive and stress tolerant based plant environments were found in locations where energy (represented by mean annual temperature) are expressed with greater weight acting on the distribution.

Elicited consequences of AMOC reduction include strong changes in temperature, precipitation distribution and sea level in the North Atlantic area.

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!).

Typical examples of pdfs include the bell - shaped normal distribution for temperature (left panel in the Fig. 1) and the exponential distribution for 24 - hr precipitation (right panel i Fig. 1).

12 Position on a Continent Distribution of Climate Regions Explain how elevation, latitude, wind systems, ocean currents, position on a continent and mountain barriers influence temperature, precipitation and distributionDistribution of Climate Regions Explain how elevation, latitude, wind systems, ocean currents, position on a continent and mountain barriers influence temperature, precipitation and distributiondistribution of climate.

9 Distribution of Climate Regions Explain how elevation, latitude, wind systems, ocean currents, position on a continent and mountain barriers influence temperature, precipitation and distributionDistribution of Climate Regions Explain how elevation, latitude, wind systems, ocean currents, position on a continent and mountain barriers influence temperature, precipitation and distributiondistribution of climate.

Changing temperature and precipitation patterns can affect the life cycle and distribution of insects, many of which transmit diseases that already pose problems to public health in Wisconsin.

This is especially true for the temperature extremes, but intensity, frequency and distribution of extreme precipitation are less well simulated.

Changing temperature and precipitation patterns can affect the lifecycle and distribution of insects, many of which transmit diseases that already pose problems for public health in Illinois.

Changing temperature and precipitation patterns can affect the life cycle and distribution of insects, many of which transmit diseases that already pose problems to public health in Pennsylvania.

To name just a few of the climate impacts of the annular modes: the NAM is associated with large anomalies in surface temperatures and precipitation across North American and Eurasia, in the distribution of sea - ice throughout the Arctic, in sea - surface temperatures over the North Atlantic, and in the spatial distribution ozone in the lower stratosphere.

HAPPI enables detailed analysis of the shifting distribution of extreme growing season temperatures and precipitation, highlighting widespread increases in extreme heat seasons and heightened skewness toward hot seasons in the tropics.

Using an ensemble of four high resolution (~ 25 km) regional climate models, this study analyses the future (2021 - 2050) spatial distribution of seasonal temperature and precipitation extremes in the Ganges river basin based on the SRES A1B emissions scenario.

Changing temperature and precipitation patterns can affect the life cycle and distribution of insects, many of which transmit diseases that already pose problems to public health in California.

Changing temperature and precipitation patterns can affect the life cycle and distribution of insects, many of which transmit diseases that already pose problems to public health in West Virginia.

Changing temperature and precipitation patterns can affect the life cycle and distribution of insects, many of which transmit diseases that already pose problems to public health in New Hampshire.

Fit of EC - Earth Northern England precipitation to a normal distribution that scales with the ensemble average global mean temperature.

For example, the Climate and Health Assessment found that «rising temperatures, changing precipitation patterns, and a higher frequency of some extreme weather events associated with climate change will influence the distribution, abundance, and prevalence» of some vectors like the mosquitos that carry the West Nile virus.

Changing distributions of temperature, precipitation, and carbon dioxide could affect the potency of plant allergens, 43 and there has been an observed increase of 13 to 27 days in the ragweed pollen season at latitudes above 44 ° N. 43

These figures illustrate the way the probability distribution of future global mean temperature change under a high - emissions scenario is linked to different potential changes in temperature and precipitation at a county - level.

Seven single - site statistical downscaling methods for daily temperature and precipitation, including four deterministic algorithms [analog model (ANM), quantile mapping with delta method extrapolation (QMD), cumulative distribution function transform (CDFt), and model - based recursive partitioning (MOB)-RSB- and three stochastic algorithms [generalized linear model (GLM), Conditional Density Estimation Network Creation and Evaluation (CaDENCE), and Statistical Downscaling Model — Decision Centric (SDSM — DC] are evaluated at nine stations located in the mountainous region of Iran's Midwest.

I have compared it to water vapor levels, OLR, precipitation, rotation of the Earth, SOI, Pacific subsurface temperatures, Trade Winds, cloud patterns, precipitation, atmospheric angular momentum, the AMO, tropical / global temperatures, and the spatial distribution of those temperature changes.

To be useful in a risk context, climate change assessments therefore need a much more thorough exploration of the tails of the distributions of physical variables such as sea level rise, temperature, and precipitation, where our scientific knowledge base is less complete, and where sophisticated climate models are less helpful.

Changing climatic variables relevant to the function and distribution of plants include increasing CO2 concentrations, increasing global temperatures, altered precipitation patterns, and changes in the pattern of «extreme» weather events such as cyclones, fires or storms.

Their species distributions often are limited by thermal and salinity boundaries, which are expected to change with regional changes in temperature and precipitation.

tree growth, and hence the width and density of tree rings, depends on many factors, including the tree species and age, the availability of stored food in the tree and nutrients in the soil, the full range of climatic variables (sunshine, precipitation, temperature, wind speed, humidity); and their distribution throughout the year.»

As Bradley points out, tree growth, and hence the width and density of tree rings, depends on many factors, including the tree species and age, the availability of stored food in the tree and nutrients in the soil, the full range of climatic variables (sunshine, precipitation, temperature, wind speed, humidity); and their distribution throughout the year.

Temperature changes induced by sun and oceans drive air circulation changes which drive changes in every aspect of climate including convection, conduction, evaporation, condensation, precipitation, windiness, cloudiness, albedo and humidity as regards both quantities and distribution.

The mean average width of a tree ring in any one tree is a function of many variables including the tree species, tree age, availability of stored food carbohydrates in the tree, nutrients in the soil, and climatic factors including sunlight, precipitation, temperature, wind speed, humidity, and their distribution througnout the year even carbon dioxide availability in the atmosphere.

The mean width of a ring in any one tree is a function of many variables, including the tree species, tree age, availability of stored food within the tree and of important nutrients in the soil, and a whole complex of climatic factors (sunshine, precipitation, temperature, wind speed, humidity, and their distribution througnout the year).

Both greenhouse gases and aerosols affect the distribution of heat and rain on this planet, but they change the temperature and precipitation in different ways in different places.

Probability distributions for average future changes in surface temperature and precipitation, for instance, may be within reach, because the main processes expected to drive such changes are captured in the current generation of climate models.