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Warming of the climate system is unequivocal, and since the 1950s, many of the observed <br /> changes are unprecedented over time spans of decades to millennia. The atmosphere and ocean <br /> have warmed,the amounts of snow and ice have diminished, and sea level has risen. Each of the <br /> last three decades has been successively warmer at the Earth's surface than any preceding decade <br /> since 1850. In the Northern Hemisphere, 1983-2012 was likely the warmest 30-year period of <br /> the last 1400 years (medium confidence). The globally averaged combined land and ocean <br /> surface temperature data as calculated by a linear trend, show warming of 0.85 [0.65 to 1.06] °C, <br /> over the period 1880 to 2012. In Colorado, the statewide annual average temperatures have <br /> increased by 2.0°F and 2.5°F over the past 30 and 50 years respectively. Warming trends have <br /> been observed over this period in most parts of the state, and show that daily minimum <br /> temperatures have warmed more than daily maximum temperatures. Additionally, temperature <br /> increases have occurred in all seasons. No long-term trends in average annual precipitation(30- <br /> 50 years) have been detected across Colorado, although since 2000 the state has experienced <br /> below-average annual precipitation and snow pack. The warming trends have contributed to an <br /> earlier shift in snowmelt and peak runoff timing in spring by approximately 1 to 4 weeks. <br /> Ocean warming has dominated the increase in energy stored in the climate system, accounting <br /> for more than 90% of the energy accumulated between 1971 and 2010 (high confidence). On a <br /> global scale, the ocean warming is largest near the surface, and the upper 75 m warmed by 0.11 <br /> [0.09 to 0.13] °C per decade over the period of 1971 to 2010. More than 60% of the net energy <br /> increase in the climate system is stored in the upper ocean (0-700 m), and about 30% is stored in <br /> the ocean below 700 m (40-year period from 1971 to 2010). The rate of sea level rise since the <br /> mid-19th century has been larger than the mean rate during the previous two millennia(high <br /> confidence). Over the period 1901 to 2010, global mean sea level rose by 0.19 [0.17 to 0.21] m. <br /> It is very likely that the mean rate of global averaged sea level rise was 1.7 [1.5 to 1.9] mm yr-1 <br /> between 1901 and 2010, 2.0 [1.7 to 2.3] mm yr-1 between 1971 and 2010, and 3.2 [2.8 to 3.6] <br /> mm yr-1 between 1993 and 2010, a trend that is increasing. <br /> The driver for the buildup in heat within the climate system is best described in terms of <br /> radiative forcing (RF). The term describes the energy balance that will occur (i.e. heating (+) or <br /> cooling (-)) in units of W m-2. The total anthropogenic RF for 2011 relative to 1750 was 2.29 <br /> [1.13 to 3.33] W m-2 (includes both heating and cooling parameter estimates). For well mixed <br /> GHG's the total positive forcing is estimated to be 2.83 [2.54 to 3.12] W m-2. The largest <br /> contribution to total radiative forcing since 1750 is caused by the increase in the atmospheric <br /> concentration of CO2. Emissions of CO2 alone caused an RF of 1.82 [f 0.19] W m-2 (64%), <br /> while CH4 caused an RF of 0.48 [f 0.05] W m-2 (17%). The data highlights methane's <br /> important role as a potent greenhouse gas, given its RF value in relation to its atmospheric <br /> loading trend, approximately 556 Tg yr-1 (64% anthropogenic, 36% natural) and relatively short <br /> atmospheric lifetime (12 years). N20 has the third largest forcing of the anthropogenic gases, at <br /> 0.17 [± 0.03] W m-2 (6%). Collectively the three GHG's of concern account for approximately <br /> 87% of the positive forcing within the climate system. <br /> DOI-BLM-CO-N020-2017-0003 19 <br />