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,r <br />He <br />,q r <br />{ a <br />� 61 <br />Ilr"rH'f, <br />y <br />4 <br />Elevation <br />Weters) <br />Upland <br />3,0 <br />Z a <br />L5 <br />.a <br />Tidal <br />An <br />F160"fia of "*0000,10, W 'Sowf W410 <br />�tl a t wrirq h4gh Water, WN,ch mrd the average Hgh fide dUair U mooni grad appira4o mala�, that <br />010fi'W tunjr .y of I04 W hi m '1hij mraM,p �P a ; = . 4r gralphicAl ire "4 rlop c4ovaa, <br />a'�ra� m:Rrm��san�a� rr>�Ir� lga�r m�r�m��ae �Nr!��ramm� �L r,�r:9amm rrcamm� ,�:aaw�l r�raLra� : r�m�rr �ilar�rwa��sxrv;m� ���� "P:� "� apaa <br />�u�u.ura° ,� C� �Nlaa� ���al �' "r��ra�. 'iu4,"M�� ?� m� u'� a�� ���� N_��acN ��.ras�• �Nr� G% :,rrrY,rr� �IW. <br />ULS . Lrawiremrr m&Mai Prale r:fdnaw Acy, <br />66 Chapter 3: Projected Impacts of Climate Change in North Carolina <br />Figure 3 -8 <br />Coastal elevations <br />for North Carolina <br />based on data from <br />Titus and Wang <br />(2008). Elevation <br />values used in these <br />data are relative to <br />spring high water <br />elevations and are <br />higher than the <br />mean tide level <br />or mean sea level <br />(Source: http: // <br />maps.risingsea. <br />net /).available with <br />a vertical accuracy <br />of 20cm.) <br />