· Possible rainfall: 0 to 2 mm Chance of any rain: 50% Hunter area. Cloudy. Medium (60%) chance of showers. Light winds becoming northerly 15 to 25 km/h during the morning. Overnight temperatures falling to between 3 and 7 with daytime temperatures reaching between 12 and 17 Rainfall 70%. Sat 17 Jul. 8°C – 18°C. Mostly sunny. Rainfall 0%. Sun 18 Jul. 3°C – 16°C. Partly cloudy. Rainfall 0%. Mon 19 Jul. 5°C – 17°C. Partly cloudy. Rainfall 20%. prev. next. Authority: Website. Disclaimer and Data Sources Disclaimer. Singleton Council is not responsible, liable and cannot guarantee that any data · A LARGE pressure system that travelled from Western Australia and swept the State on Thursday provided the Singleton Local Government Area with some decent rainfall totals. All major areas received more than the predicted ten millimetres, with Singleton outshining all other areas, receiving millimetre over 24 hours. Pokolbin was not far behind, with [ ]
Weather - Australia 7 day forecasts and weather radar - Weatherzone
Global average temperature has increased by about 1, singleton rainfall. With singleton rainfall reductions in emissions, global temperature increase could be limited to 3. Without significant reductions, annual average global temperatures could increase by 9°F 5°C or more by the end of this century compared to preindustrial temperatures.
Increasing sea surface temperatures, rising sea levels, and changing patterns of precipitation, winds, nutrients, and ocean circulation are contributing to overall declining oxygen concentrations in many locations, singleton rainfall.
Global average sea level has risen by about 7—8 inches about 16—21 cm sincewith almost half this rise occurring since as oceans have warmed and land-based ice has melted. Relative to the yearsea level is very likely to rise 1 to 4 feet 0. Emerging science regarding Antarctic ice sheet stability suggests that, for higher scenarios, a rise exceeding 8 feet 2. Annual average temperature over the contiguous United States has increased by 1. Additional increases in annual average temperature of about 2.
Annual precipitation since the beginning of the last century has increased across most of the northern and eastern United States and decreased across much of the southern and western United States.
Over the coming century, significant increases are projected singleton rainfall winter and spring over the Northern Great Plains, the Upper Midwest, and the Northeast. Observed increases in the frequency and intensity of heavy precipitation events in most parts of the United States are projected to continue, singleton rainfall.
Surface soil moisture over most of the United States is likely to decrease, accompanied by large declines in snowpack in the western United States and shifts to more winter precipitation falling as rain rather than snow.
In the Arctic, annual average temperatures have increased more than twice as fast as the global average, accompanied by thawing permafrost and loss of sea ice and glacier mass, singleton rainfall. Arctic-wide glacial and sea ice loss is expected to continue; by mid-century, it is very likely that the Arctic will be nearly free of sea ice in late summer.
Permafrost is expected singleton rainfall continue to thaw over the coming century as well, singleton rainfall, and the carbon dioxide and methane released from thawing permafrost has the potential singleton rainfall amplify human-induced warming, possibly significantly. Human-induced change is affecting atmospheric dynamics and contributing to the poleward expansion of the tropics and the northward shift in Northern Hemisphere winter storm tracks since Increases in greenhouse gases and decreases in air pollution have contributed to increases in Atlantic hurricane activity since Regional changes in sea level rise and coastal flooding are not singleton rainfall distributed across the United States; ocean circulation changes, sinking land, and Antarctic ice melt will result in greater-than-average sea level singleton rainfall for the Northeast and western Gulf of Mexico under lower scenarios and most of the U.
coastline other than Alaska under higher scenarios. Since the s, sea level rise has already increased the frequency of high tide flooding by a factor of 5 to 10 for several U. coastal communities. The climate change resulting from human-caused emissions of carbon dioxide will persist for decades singleton rainfall millennia.
Future changes outside the range projected by climate models cannot be ruled out, and due to their systematic tendency to underestimate temperature change during past warm periods, models may be more likely to underestimate than to overestimate long-term future change, singleton rainfall.
Documenting Uncertainty: This assessment relies on two metrics to communicate the degree of certainty in Key Findings. See Guide singleton rainfall this Report for more on assessments of likelihood and singleton rainfall. Wuebbles, singleton rainfall, D. Easterling, D. Fahey, S. Doherty, J. Kossin, W. Sweet, R. Vose, and M. Wehner, Our Changing Climate. Singleton rainfall, D. Easterling, K. Kunkel, K, singleton rainfall.
Lewis, T. Maycock, and B. Stewart eds, singleton rainfall. Global Change Research Program, singleton rainfall, Washington, DC, USA, pp. doi: This chapter is based on the Climate Science Special Report CSSRwhich is Volume I of the Fourth National Climate Assessment available at science The Key Messages and the majority of the content represent the highlights of CSSR, updated with recent references relevant to these topics.
The interested reader is referred to the relevant chapter s in CSSR for more detail on each of the Key Messages that follow. Long-term temperature observations are among the most consistent and widespread evidence of a warming planet, singleton rainfall. Global annually averaged temperature measured over both land and oceans has increased by about 1. The last few years have also seen record-breaking, singleton rainfall, climate-related weather extremes. For example, since the Third National Climate Assessment was published, 1 became the warmest year on record globally; surpassed by a wide margin; and surpassed For short periods of time, from a few years to a decade or so, the increase in global temperature can be temporarily slowed or even reversed by natural variability see Box 2.
Over the past decade, such a slowdown led to numerous assertions that global warming had stopped, singleton rainfall. No temperature records, however, show that long-term global warming has ceased or even substantially slowed over the past decade. Observed trends have been confirmed by multiple independent research groups around the world.
Many lines of evidence demonstrate that human singleton rainfall, especially emissions of greenhouse gases from singleton rainfall fuel combustion, singleton rainfall, deforestation, and land-use change, are primarily responsible for the climate changes observed in the industrial era, especially over the last six decades.
Observed warming over the period — was 1. By absorbing the heat emitted by Earth and reradiating it equally in all directions, greenhouse gases increase the amount of heat retained inside the climate system, warming the planet.
Aerosols produced by burning fossil fuels and by singleton rainfall human activities affect climate both directly, by scattering and absorbing sunlight, as well as indirectly, through their impact on cloud formation and singleton rainfall properties. Over the industrial era, the net effect of the combined direct and indirect effects of aerosols has been to cool the planet, partially offsetting greenhouse gas warming at the global scale.
Over the last century, changes in solar output, volcanic emissions, and natural variability have only contributed marginally to the observed changes in climate Figure 2.
Click legend item names to toggle graph lines. View static image, singleton rainfall. While there are uncertainties associated with modeling some of these feedbacks, 2425 the most up-to-date scientific assessment shows that the net effect of these feedbacks over the industrial era has been to amplify human-induced warming, singleton rainfall, and this amplification will continue over coming decades 18 see Box 2.
With significant reductions in emissions of greenhouse gases, the future rise in global average temperature could be limited to 3. For this reason, it is essential to highlight the fact that observed changes in the global average temperature of the atmosphere represent only a small fraction of total warming.
This carbon uptake is making near-surface ocean waters more singleton rainfall, which in turn can harm vulnerable marine ecosystems see Ch. Although tropical coral reefs are the most frequently cited casualties of ocean warming and acidification, ecosystems at higher latitudes singleton rainfall be more vulnerable than those at lower latitudes as they typically have a lower buffering capacity against changing acidity.
Regionally, singleton rainfall, acidification is greater along the U. coast than the global average, as a result of upwelling for example, in singleton rainfall Pacific Northwestchanges in freshwater inputs such as in the Gulf of Maineand nutrient input as in urbanized estuaries.
In addition to higher temperatures and increasing acidification, ocean oxygen levels are also declining in various ocean locations and in many coastal areas. Over the last 50 years, declining oxygen levels have been observed in many inland seas, estuaries, and nearshore coastal waters, singleton rainfall. Byunder a higher scenario RCP8. Rising Global Sea Levels Global average sea level has risen by about 7—8 inches about 16—21 cm sincewith almost half this rise occurring since as oceans have warmed and land-based ice has melted.
Sinceglobal average sea level has risen by about 7—8 inches about 16—21 cm. The rate of sea level rise over the 20th century was higher than in any other century in singleton rainfall least the last 2, years, according to proxy data such as salt marsh singleton rainfall and fossil corals. Over the first half of this singleton rainfall, the singleton rainfall scenario the world follows has little effect on projected sea level rise due to the inertia in the climate system.
However, the magnitude of human-caused emissions this century significantly affects projections for the second half of the century and beyond Figure 2. Relative to the yearglobal average sea level is very likely to rise by 0. Several avenues of research, including emerging science on physical feedbacks in the Antarctic singleton rainfall sheet e. Regardless of future scenario, singleton rainfall, it is extremely likely that global average sea level will continue to rise beyond Increasing U.
Temperatures Annual average temperature over the contiguous United States singleton rainfall increased by 1. Over the contiguous United States, annual average temperature has increased by 1.
At the regional scale, each National Climate Assessment NCA region experienced an overall warming between — and — Figure 2. The largest changes were in the singleton rainfall half of the United States, where average temperature increased by more than 1.
Over the entire period of record, the Southeast has had the least singleton rainfall due to a singleton rainfall of natural variations and human influences; 87 since the early s, however, the Southeast has singleton rainfall warming at an accelerated rate, singleton rainfall.
Over the past two decades, the number of high temperature records recorded in the United States far exceeds the number of low temperature records. The length of the frost-free season, from the last freeze in spring to the first freeze of autumn, has increased for all regions since the early s, singleton rainfall.
Over timescales shorter than a decade, the s Dust Bowl remains the peak period for extreme heat in the United States for a variety of reasons, including exceptionally dry springs coupled with poor land management practices during that era. Singleton rainfall the next few decades, annual average temperature over the contiguous United States is projected to increase by about 2.
As a result, recent record-setting hot years are projected to become common in the near future for the United States. Much larger increases are projected by late century: 2. Extreme high temperatures are projected to increase even more than average temperatures. Cold waves are projected to become less intense and heat waves more intense. The number of days below freezing is projected to decline, while the number of days above 90°F is projected to rise.
Changing U. Precipitation Annual precipitation since the beginning of the last century has increased across most of the northern and eastern United States and decreased across much of the southern and western United States. In summer, a slight decrease is projected across the Great Plains, with little to no net change in fall, singleton rainfall. The frequency and intensity of heavy precipitation events across the United States have increased singleton rainfall than average precipitation Figure 2.
These trends are consistent with what would be expected in a warmer world, as increased evaporation rates lead to higher levels of water vapor in the atmosphere, which in turn lead to more frequent and intense precipitation extremes.
Our Changing Climate - Fourth National Climate Assessment
· Singleton climatology including monthly and daily averages and records of temperature and rain · Singleton daily rain summaries including extremes, records and averages as well as archived historical data Singleton minimum temp history (°S, °E, 32m AMSL) Coldest ever° 09/07/ Coldest this year° 06/07/ Coldest this month
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