Over Greenland, temperature Patient has risen significantly Degree since the early 1990s Duration , reaching values similar to those in the 1930s (Box et al., 2009). [ WG1AR5DD 0 MCLH 16/03/2014 ]

Should sea emissions for Annex I countries Patient rise during the 1990s Duration , then fall to the 1990 level in the year 2000, the increase in concentration in the year 2000 would be approximately 0.4 ppmv for every additional GtC of CO2 emissions accumulated over 1990 - 2000 declining to 0.2 ppmv per additional GtC by 210010. [ 6IPCCEMISSIONS 0 TK MCLH 20/07/2012 ]

Nitrate aerosols continue to increase through 2100 as ammonia emissions Patient rise steadily Duration due to increased use of agricultural fertilizer Cause even as all other aerosol precursor emissions decrease (Figure 8.2), including sulphur dioxide which drives the reduction in sulphate aerosol that also contributes to additional formation of nitrate aerosols in the future (Bauer et al., 2007; Bellouin et al., 2011). [ WG1AR5HW 0 MCLH 16/03/2014 ]

If emissions for Annex I countries Patient rose over the 1990s Duration so that their level in the year 2000 exceeded that in 1990 and the higher 2000 level (or some other level) was used as a baseline for future reductions in Annex I country emissions, this would also affect future concentrations. [ 6IPCCEMISSIONS 0 TK MCLH 20/07/2012 ]

Hotter temperatures at the surface and higher humidity levels will also make the air in thunderstorm cells Patient rise faster Manner and higher Degree , creating more dynamic storm clouds and more powerful storms. [ 2CANADACCD9801 0 TK MCLH 20/07/2012 ]

Furthermore, the large ice sheets that store vast quantities of water as ice covering Greenland and Antarctica are expected to slowly release this water into the oceans if global temperatures Patient rise significantly Degree . [ 5CANADAICC 0 TK MCLH 20/07/2012 ]

As annual temperatures Patient rise over the long-term Duration due to global warming Cause , for example, non-native plant, insect and animal species may more easily invade new ecosystems where there is often no check on their behaviour. [ AWORLDOFSCIENCE 0 TK MCLH 20/07/2012 ]

When temperatures Patient rise , evaporation from surface waters also becomes greater and the water cycle becomes more active. [ 1CANADACCD 0 TK 20/07/2012 ]

As temperatures Patient rise , the extent of snow and sea ice cover in the Northern Hemisphere will decrease. [ 5CANADAICC 0 TK 20/07/2012 ]

In the three GHG + A experiments, temperatures over land masses Patient rise , on average, by 2.5 ° C Value by 2050 Time , while ocean temperatures warm by 1.5 ° C. [ 3CANADAENVIRON 0 TK MCLH 16/03/2014 ]

For emissions limitation cases where non-Annex I countries follow IS92a and IS92e, global emissions over land masses Patient rise continuously through the twenty-first century Duration (see Figure 4). [ 6IPCCEMISSIONS 0 TK MCLH 14/03/2014 ]

This process Cause makes the temperature Patient rise in the atmosphere Location just as it does in the greenhouse. [ ENCY 0 TK 20/07/2012 ]

Since the 1960s in the Southern Hemisphere but after 1975 in the Northern Hemisphere, temperatures Patient have risen sharply Manner . [ ENCY 0 TK MCLH 16/03/2014 ]

Temperatures Patient have risen during the past four decades Duration in the lowest 8 kilometres of the atmosphere Location . [ GREENFACTS 0 TK MCLH 16/03/2014 ]

The large-scale drying in the Mediterranean, southwest USA, and southern Africa appear across generations of projections and climate models and is deemed likely as global temperatures Patient rise and will increase the risk of agricultural drought. [ WG1AR5NK 0 MCLH 16/03/2014 ]

In summer under strong sunshine, the temperature on land Patient rises much more quickly Manner than the temperature at the sea surface. [ AWORLDOFSCIENCE 0 TK MCLH 16/03/2014 ]

Global mean temperatures Patient will continue to rise over the 21st century Duration if greenhouse gas (GHG) emissions continue unabated Condition . [ WG1AR5MW 0 MCLH 16/03/2014 ]

It is very likely that NH snow cover will reduce as global temperatures Patient rise over the coming century Duration . [ WG1AR5MW 0 MCLH 16/03/2014 ]

It is very likely that temperatures Patient will continue to rise over New Zealand Location . [ WG1AR5OZ 0 MCLH 16/03/2014 ]

Consequently, sea levels Patient can rise by several hundred metres Value , covering large areas of the continents with warm shallow seas. [ ENCY 0 TK 20/07/2012 ]

Sea level Patient could rise if the effects of marine instability become important Condition , but there is not enough evidence at present to unambiguously identify the precursor of such an unstable retreat. [ WG1AR5OG 0 MCLH 16/03/2014 ]

Another complication is that the sea level over land masses Patient would not rise by the same amount Value all over the globe Location due to the effects of the Earth 's rotation, local coastline variations, changes in major ocean currents, regional land subsidence and emergence, and differences in tidal patterns and sea water density Cause . [ ENCY 0 TK MCLH 20/07/2012 ]

If the huge Greenland ice sheet melts, which might happen over the next few centuries, sea levels Patient could rise by as much as seven metres Value . [ CHANG_CLIMATECHANGEYOUTH 0 TK 20/07/2012 ]

The mean levels of the world 's seas Patient have been rising slowly Manner over the past 100 years Duration by several hundred metres at a rate of 1.5 cm each decade Value . [ 5CANADAICC 0 TK 20/07/2012 ]

As the ice caps melt, sea levels rise. They Patient have already gone up by 10 - 25 centimetres over the last century (depending on the measurement) and are projected to rise further by up to 88 centimetres Value by 2100 Time . [ CLIMATECHANGEYOUTH 0 TK 20/07/2012 ]

Results since the AR4 show that for recent decades, sea level Patient has continued to rise (Section 3.7). [ WG1AR5NZ 0 MCLH 16/03/2014 ]

Consistent with this energy accumulation, global mean sea level Patient has continued to rise during 1998-2012 Duration , at a rate only slightly and insignificantly lower than during 1993-2012 Manner (Section 3.7). [ WG1AR5JW 0 MCLH 16/03/2014 ]

These and natural forces have contributed to changes in the Earth 's climate over the 20th century: Land and ocean surface temperatures have warmed, the spatial and temporal patterns of precipitation have changed, sea level Patient has risen , and the frequency and intensity of El Nino events have increased. [ 2IPCCBIODIVERSITE 0 TK 20/07/2012 ]

This included the recognition that sea level Patient had risen during the 20th century Duration . [ WG1AR5NY 0 MCLH 16/03/2014 ]

All of the previous IPCC assessments have projected that global sea level Patient will continue to rise throughout this century Duration for the scenarios examined. [ WG1AR5AV 0 MCLH 16/03/2014 ]

Global mean sea level Patient will continue to rise during the 21st century Duration (see Figure SPM.9). [ WG1AR5AF 0 MCLH 16/03/2014 ]

Global average sea level Patient has risen and ocean heat content has increased. [ GREENFACTS 0 TK 20/07/2012 ]

Global mean sea level (GMSL) Patient has risen by 0.19 [0.17 to 0.21] m Value over the period 1901-2010 Duration , calculated using the mean rate over these 110 years, based on tide gauge records and since 1993 additionally on satellite data. [ WG1AR5CI 0 MCLH 16/03/2014 ]

Sea level Patient can rise or fall on time scales ranging from hours to centuries Duration , spatial scales from 1 km to global Expanse , and with height changes from a few millimeters to a meter or more (due to tides) Value . [ WG1AR5CL 0 MCLH 16/03/2014 ]

The atmosphere and ocean have warmed, the amounts of snow and ice have diminished, sea level Patient has risen, and the concentrations of greenhouse gases have increased (see Figures SPM.1, SPM.2, SPM.3 and SPM.4). [ WG1AR5AB 0 MCLH 16/03/2014 ]

It is likely that most of this rise in sea level Patient has been due to the increase in global temperature over the last 100 years. [ CHANG_ENCY 0 TK 20/07/2012 ]

The estimated multiplication factor (shown at tide gauge locations by colored dots), by which the frequency of flooding events of a given height increase for (a) a mean sea level (MSL) Patient rise of 0.5 m Value (b) using regional projections of MSL for the RCP4.5 scenario, shown in Figure13.19a. [ WG1AR5OM 0 MCLH 16/03/2014 ]

Many countries, especially Egypt, Vietnam, Japan, etc., would be extremely vulnerable to a rise in sea level Patient , reduction in food production and loss of land is projected. [ CHANG_3CANADAENVIRON 0 TK 20/07/2012 ]

Global mean sea level (GMSL) Patient rise (metres) projected by semi-empirical models and compared with the IPCC AR4 and AR5 projections. [ WG1AR5OH 0 MCLH 16/03/2014 ]

There are, however, significant interannual and decadal-scale fluctuations about the average rate of sea level Patient rise in all records. [ WG1AR5CL 0 MCLH 16/03/2014 ]

A rise in sea level Patient will have a serious impact on atoll agroforestry and the pit cultivation of taro which are important for many island communities. [ CHANG_2IPCCBIODIVERSITE 0 TK 20/07/2012 ]

The Greenland ice sheet Cause has contributed to a rise in global mean sea level Patient over the last few decades Duration , and this trend is expected to increase during this century. [ WG1AR5OG 0 MCLH 16/03/2014 ]

In both cases, the maximum of the histogram is slightly higher than the GMSL, whereas the arithmetic mean is lower. Only some coastlines will experience a sea level Patient rise of up to about 40 % above GMSL change Value . [ WG1AR5OL 0 MCLH 16/03/2014 ]

The strong physical relationship between thermosteric sea level and ocean heat content (through the equation of state for seawater) means that the anthropogenic ocean warming Cause (Section 10.4.1) has contributed to global sea level Patient rise over this period Duration through thermal expansion Method . [ WG1AR5LO 0 MCLH 16/03/2014 ]

The results (Figure 10) show a rise in average global sea level Patient due to thermal expansion of approximately 5 cm during the twentieth century and an additional rise of 40 cm by the last two decades of the twenty-first century. [ CHANG_3CANADAENVIRON 0 TK MCLH 20/07/2012 ]

A rise in mean sea level Patient can explain most of the increase in extreme sea levels: [ WG1A55CI 0 MCLH 16/03/2014 ]

The rise in mean sea level Patient can explain most of the observed increase in extreme sea levels (Figure 3.15). [ WG1AR5CQ 0 MCLH 16/03/2014 ]

Most of the increase in extreme sea level can be explained by the mean sea level Patient rise: changes in extreme high sea levels are reduced to less than 5 mm yrÐ1 at 94% of tide gauges once the rise in mean sea level is accounted for. [ WG1AR5AJ 0 MCLH 16/03/2014 ]

Second, sea level Patient rise adds to the heights of sea level extremes, regardless of any changes in the storm-related component. [ WG1AR5CM 0 MCLH 16/03/2014 ]

However, sea level Patient rise due to changes in ocean mass Cause enhances clathrate stability in the ocean. [ WG1AR5AL 0 MCLH 16/03/2014 ]

For coastal planning, sea level Patient rise needs to be considered in a risk management framework, requiring knowledge of the frequency of sea level variability (from climate variability and extreme events) in future climates, projected changes in mean sea level, and the uncertainty of the sea level projections (Hunter, 2010, 2012), as well as local issues such as the compaction of sediments in deltaic regions and the changing supply of these sediments to maintain the height of the deltas (Syvitski et al., 2009). [ WG1AR5OM 0 MCLH 16/03/2014 ]

Whilst scientists believe this to reflect mostly regional changes in climate, the recent summertime disintegration of the Larsen Ice Shelf has renewed speculation that climatic changes in the polar regions have the potential to cause severe impacts via a rise in global sea level Patient over the next 100 to 200 years Duration . [ CHANG_ENCY 0 TK MCLH 20/07/2012 ]