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C Sea-level rise

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C ijA gCMcCB Sea level rise (deference to you bed-wetting) is a phenomenon that the rise in sea levels in the expansion and the heat of the seawater due to global warming.

Contents

[ W ] NC The recent rise in sea level

CeA FlcBAssA IZAjAA[A }[Vy80%v\B Impact of sea level rise, particularly in cities such as Venice, a small island nation in Oceania and has become a serious problem, Islands Marshall is 80 percent of the country are expected to sink. I_ A oOfVACCnLssdvB The Netherlands and Tokyo, as part and in Bangladesh, it is important for nations and cities in coastal areas below sea level. oOfVy18%B Bangladesh in particular, 18 percent of the land is said to have been lost.

[ W ] C Causes of sea level rise

CCMcAXZ A O[h XZB The main cause of rising sea levels and expansion of the thermal waters, followed by melting of glaciers, which give the floor is melting ice in Greenland. PMcZAClAvUlAIfKvB Not rise by thermal expansion and melting just thinking on the decline or rise in sea level, considered separately once a couple of factors need to be a comprehensive summary of them.

  • kCCCXZ : CXAXRnWZxCB Sea ice melting and sea Antarctic and Ocean Arctic: a lot of sea ice, can lower the concentration of salt from sea water by a freshwater inflow of melting glaciers and the inflow from rivers and coastal land. oACXZxACZxB Since the salt coagulation and precipitation, and salinity of sea ice is very thin, less than the concentration in seawater. AxCXB Therefore, sea ice is the density difference increases. Zx=xEAkCZiCZxAZiiZCB The rise of salinity difference being that depends on the density difference, especially in the Arctic Ocean to the lower salinity of the seawater itself forward as the melting, sea levels rise as per the amount of melting to go on record a lower melting .
  • kXRZ : XRXRACo_X9xCAZZxCB Melting glaciers in Antarctica and the Arctic: the case of an iceberg of glacial origin, the volume of the glaciers at the sea from landREoTA volume increased 9 percent less than sea level, after only a few minutes to melt the sea level difference of more salt increase the volume.
  • k AxnARXEcXEivyZ : ZCoACB Antarctica and the Arctic, high-latitude regions, permafrost melting snow remaining glaciers in the alpine:REoTA minutes in sea water and the melting, the increase in volume of the sea.
  • C : XoACB Seawater inflow to the other: If the lake bottom of glacial runoff on the land, increase the volume of water volume only. AXyAZCC}lB Also, if there is sediment in the glacial water masses and the possibility that a sudden increase in volume flowing into the sea off with the melting.
  • Mc : xMcA4xIB Expansion heat: the thermal expansion at different rates depending on temperature, 4 C volume off if the increase in acceleration fromRERE.
  • : CACB Amount of evaporation: changes in the amount of evaporation from the sea, the sea change the volume. I~WB Are related to the amount of precipitation and indirectly.
  • n` : ACN~ARyACn`CB Changes in the landscape: even if the volume does not change, uplift and subsidence of the seabed, and deposition of sediment derived from land, by sea level rise, changes in the terrain that borders the sea.

2100NC\A IPCC3(2001)9`88cm A 4 (2007)A18`59cmi[1] jB 2100 prediction of the amount of sea level rise by the year, IPCC's third report (2001) 9 ~ 88cm rise in the minimum of the fourth report (2007), a minimum of 18 ~ 59cm and the rise of (this is only present in lower [1]). IPCCfO[hXox\lANKZoxAl[2] B But the IPCC models do not take into account the possibility of accelerating the rate of glacier runoff and the extreme southwest of Greenland, is also observed in recent years been observed to accelerate the rate of snowmelt runoff and a large real As is evidentSA numbers to exceed the amount of this increase [2]. 2009N2WMOy[XXZACIPCClAI80cmBwE[3] B WMO, 2009 and in February with a report of faster melting of glaciers in western Antarctica and the Antarctic Peninsula, the amount of sea level rise than the IPCC value of the up to 80cm during this century to reach a risk have pointed out [3]. #XZQB # See also the melting of the floor, ice, Antarctica.

[ W ] XC sea level rise since the Ice Age

  • OXBC16000NIAC100[gOB Ice age the last time around the end BC16000, when the sea level lower than currently around 100 meters.
  • BC12000C}nA8000NBC4000N100[gCxB BC12000 starts from the sharp rise in sea level around 8,000 years to around 100 in BC4000 close to current levels and rising sea levels meters.
  • BC9200NBC8000N1200NrICxA45[gB Since BC9200 and BC8000 until around 1200 when a relatively stable level as the sea level, which is now 45 meters lower.
  • BC6000NA30[gxB BC6000 around, much lower than the current 30 meters.
  • BC4000NCs[NBA[gCB BC4000 peak height of the sea surface around this time the sea level several meters higher than now. BC2500NB This lasted until around BC2500. {4[gB In Japan is now in the era when the study of Jomon four meters high. [1]100kmCB [1] in the plains there is some 100km inland location is the current shoreline. ACACiA{CiB In the current, which was seen as the rising sea level, it was going towards the sea to land in Japan is called the Jomon onlap.
  • AC[g3JB Then, a few meters of sea level in the range three times up and down repeatedly.
  • rIxB Current level is relatively high.

[ W ] Ce Impact of sea level rise

Cn[eB Sea level rise will cause serious impact to the groundwater. ICZAHpp^A OnB And the direct alteration of water seeping from the sea, the first example may be difficult to use water for industrial water and drinking, ie, the rise of the groundwater level have been surprisingly overlooked . nxbAB More buoyancy to the part time basis to support the ground and buildings in other words, they boost. eSonArbXQnB Effects are already starting to focus on coastal areas, have begun to cause damage and that the foundation of the building tilted toKIGA.

[ W ] XZ melting of Antarctic ice sheet

XngeAZ~AX\wE[2] B About the effect of warming the earth of the floor of the Antarctic ice is melting exceed the amount of precipitation was could not reduce the ice sheet [2]. _ngCi ng^_#XZQjB Deny the claim were taken by sea-level rise and global warming to the theory of cold reasoning (skeptic on global warming # additional melting glaciers). O[hXZxs_cA IPCC4] (AR4)IC\l[1] B The rate of melting of the Greenland and Antarctic ice sheets, however, is left for questions, IPCC Fourth Assessment Report (AR4) for amount of rise in sea level this century, but not only on the lowest estimate of the amount [1]. AR4AX\z}ZwEA2006N10NXLZx59¬Xx2003N10N12%[1] [4] [5] [6] B But since AR4, been several reports have been melting faster than expected in the Antarctic ice sheet, melting speeds up to 10 years in a wide area of the West Antarctic Ice Sheet at 59 percent annuallyMAand that the rate of sea ice falling from 10 in 2003, and 12 percent were found to be accelerated [1] [4] [5] [6]. \KZ[7] B The phenomenon has been observed above the major snowmelt also predicted [7]. IPCCLCO[2] B This IPCC is concerned that the significant increase in the amount of sea level rise than are listed in the report [2]. X(WAIS)CA]\ZZ6mC\wE[8] B Antarctic Ice Sheet also southwest (WAIS) is due toRIKOMI under water, up to melting in the short term prediction of the traditional than 6m has been pointed out can cause a rise in sea level [8]. AIPCCwEo[9] B Recent observations by those present that the IPCC has also been tense over the situation reported [9].

[ W ] oT Source

  1. ^ a b c uEvViIAXZAAFPA2008N0114 ^ A b c "The last day of world" scenario, the accelerated melting of ice sheets in Antarctica, AFP, 2008 years January 14
  2. ^ a b c kEX@E}(08/01/28) ^ A b c of the emergency response toward long-term stability of the Antarctic ice over the Arctic crisis (08/01/28)
  3. ^ Fgg@C@vlnAVA2009N226 ^ Antarctic: sea-level rise acceleration and expansion of the WMO Global Warming Report, Mainichi Shimbun, 2009 February 26
  4. ^ Eric RignotARecent Antarctic ice mass loss from radar interferometry and regional climate modellingANature Geoscience 1, 106-110 (2008) iLLeoTj ^ More Eric Rignot, Recent Antarctic Ice Loss from radar interferometry and mass Regional climate modeling, Nature Geoscience 1, 106-110 (2008) (Source of article above)
  5. ^ Antarctic glaciers 'flow faster', BBC, 6 June 2007 ^ Antarctic glaciers' Flow faster ', BBC, 6 June 2007
  6. ^ "Buried Lakes Send Antarctica's Ice Slipping Faster Into the Sea, Study Shows", National Geographic, 2007N221 ^ "Buried Lakes Send Antarctica's Ice Slipping Faster Into The Sea, Study Shows", National Geographic, 2007 Sunday February 21 years
  7. ^ KZ geiVA2007N 527j ^ I found the impact of global warming and snow melting in the unusual situation of Antarctica (Asahi Shimbun, 2007 May 27)
  8. ^ Huge sea level rises are coming – unless we act now, New ScientistA2007N725 ^ Huge sea level rises are Coming - unless We act now, New Scientist, July 25 years 2007
  9. ^ GO A{ YfViIAHVA ISBN 978-4-526-06090-8 AP.188 ^ Nishioka Hidezou, low-carbon society scenarios Japan, Nikkan Kogyo Shimbun, ISBN 978-4-526-06090-8, p.188

[ W ] A See also


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