{"text_format":"2","workbook":"xls","n_sheets":1,"sheets":["調査結果"],"not_rendered":{"charts":0,"images":0,"macros":0,"external_links":1,"defined_names":0,"comments":0,"pivot_tables":0},"unopened":[],"bounds":{"document_bytes":16777216,"sheet_cells":100000,"run_cost":"one","rows_first":2000,"rows_last":500,"rows_between":2000,"halvings":0,"cell_chars":16384,"cell_head_chars":4096},"cells_cut":0,"cells_raw":0,"read":"whole","date_system":"1904","formulas":"cached_only"}

{"sheet":"調査結果","index":0,"n_rows":31,"n_cols":24,"rows_kept":31,"cut":false,"hidden":false,"merged":[[1,9,2,9],[1,13,2,13],[1,14,2,14],[1,15,2,15],[1,19,1,20],[0,16,2,16],[0,17,2,17],[0,18,0,23],[0,0,2,0],[0,1,0,15],[1,1,2,1],[1,2,1,4],[1,5,1,7],[1,8,2,8]],"flags":["formulas_cached_only"]}
["地点番号","現地調査",{"$nulls":14},"調査グループ","備考","潮位補正"]
[null,"地名","北緯",null,null,"東経",null,null,"年/月/日","時刻","測定高","津波高","汀線からの","測定対象","根拠","信頼度*2",null,null,"測定時の","最大波発生日時（予想）",null,"最大波発生時（予想）","潮位補正の","潮位補正後の高さ"]
[null,null,"度","分","秒","度","分","秒",null,null," a (m)","の種類*1","測定距離 (m)",{"$nulls":5},"潮位 b (m)","年/月/日","時刻","の潮位 c (m)","参照地点","a+b-c (m)"]
[104,"千葉県旭市下永井",35,41,33.98,140,44,18.09,"2011-04-13","10:40:00",7.614,"R",null,"ススキ原の漂着ごみ","漂流物","A","気象研","第一波が最大と推定",0.098,"2011-03-11","15:40:00",-0.442,"銚子漁港",8.154]
[101,"千葉県旭市下永井",35,41,39.75,140,44,4.96,"2011-04-12","12:00:00",3.253,"I",null,"海匝漁協地方卸売市場のガラス窓","浸水痕","A","気象研","第一波が最大と推定。飯岡灯台から撮影されたビデオの15時40分頃の状況と、測定した場所の浸水がほぼ同じ高さだと、映像から判断できることによる。",-0.102,"2011-03-11","15:40:00",-0.442,"銚子漁港",3.5930000000000004]
["105A","千葉県旭市下永井",35,41,32.83,140,43,45.35,"2011-04-13","11:00:00",2.573,"I",null,"公園のトイレ内壁","浸水痕","C","気象研","地点番号105Bの低い方の列と近い測定高であることから、より上部に浸水した痕跡が逸失していて、より低い後続波の痕跡を測定している可能性が十分に考えられるため、信頼度は低い。",0.098,"2011-03-11","15:40:00",-0.442,"銚子漁港",3.113]
["105B","千葉県旭市下永井",35,41,32.8,140,43,43.43,"2011-04-13","11:00:00",3.043,"R",null,"みなと公園内の斜面","漂流物","A","気象研","第一波が最大と推定。より低い場所にもう一列（測定高で0.42m低い）の漂着物の列があり、これが後続波の遡上点と考えられる。",0.098,"2011-03-11","15:40:00",-0.442,"銚子漁港",3.583]
[106,"千葉県旭市下永井",35,41,37.8,140,43,35.02,"2011-04-13","11:30:00",4.31,"I",null,"屋台型クレープハウスの外壁","浸水痕＋目撃証言","A","気象研","第一波が最大と推定。測定高は海岸堤防上面+0.09m。",0.078,"2011-03-11","15:40:00",-0.442,"銚子漁港",4.83]
["107A","千葉県旭市西下町",35,41,40.53,140,43,31.29,"2011-04-13","12:00:00",5.401,"I",null,"民家の外壁","浸水痕","A","気象研","第三波が最大。薄暗くなってからの第三波の方が第一波よりも高かったとの証言による。",0.058,"2011-03-11","17:30:00",-0.167,"銚子漁港",5.6259999999999994]
["107B","千葉県旭市西下町",35,41,43.18,140,43,30.24,"2011-04-13","12:00:00",5.335,"I",null,"民家の車庫の内壁","浸水痕","A","気象研","第三波が最大と推定",0.058,"2011-03-11","17:30:00",-0.167,"銚子漁港",5.56]
[108,"千葉県旭市平松",35,42,3.48,140,43,13.27,"2011-04-13","13:25:00",6.162,"I",null,"民家の外壁","浸水痕＋目撃証言","A","気象研","第三波が最大と推定、最大波の推定は伝聞による。",0.062,"2011-03-11","17:30:00",-0.167,"銚子漁港",6.391]
[109,"千葉県旭市横根",35,42,9.05,140,42,51.73,"2011-04-13","14:35:00",5.931,"I",null,"機械作業場の外壁","浸水痕＋目撃証言","A","気象研","第三波が最大と推定。測定高は海岸堤防上面+1.42m、一波目よりも二波目が高く、その後も津波が堤防を越えたとの証言があるが、最大波発生時刻は不明。",-0.208,"2011-03-11","17:30:00",-0.167,"銚子漁港",5.89]
[110,"千葉県旭市三川",35,42,8.54,140,42,20.26,"2011-04-13","15:20:00",6.045,"I",null,"民家の外壁","浸水痕＋伝聞","A","気象研","第一波が最大と推定",-0.309,"2011-03-11","15:40:00",-0.442,"銚子漁港",6.178]
[111,"千葉県旭市三川",35,42,6.1,140,41,35.1,"2011-04-13","16:30:00",5.78,"I",null,"民家のガラス戸","浸水痕","A","気象研","第一波が最大。調査点の東0.2kmの店舗で、第一波に店先に浸水した箇所より高い所には、その後の津波で浸水した形跡がない、という目撃証言。",-0.402,"2011-03-11","15:40:00",-0.442,"銚子漁港",5.82]
[102,"千葉県旭市三川",35,41,55.94,140,41,16.21,"2011-04-12","16:30:00",7.889,"R",null,"防潮林に絡まった枯れ草","漂流物＋目撃証言","A","気象研","第一波が最大。津波が来たのは一回だけで16時より前だったとの証言による。",-0.552,"2011-03-11","15:40:00",-0.442,"銚子漁港",7.779]
["103A","千葉県旭市中谷里",35,41,11.57,140,38,58.17,"2011-04-12","17:20:00",5.417,"I",null,"民家の外壁","浸水痕","A","気象研","第一波が最大と推定",-0.549,"2011-03-11","15:40:00",-0.442,"銚子漁港",5.31]
["103B","千葉県旭市中谷里",35,41,11.13,140,39,0.03,"2011-04-12","17:20:00",5.749,"I",null,"公園のトイレ内壁","浸水痕","A","気象研","第一波が最大と推定",-0.549,"2011-03-11","15:40:00",-0.442,"銚子漁港",5.6419999999999995]
[]
[]
[]
["*1 津波高の種類",{"$nulls":15},"氏　名","所　属"]
["　　R: 遡上高",{"$nulls":15},"○前田　憲二","気象研究所地震火山研究部"]
["　　I: 浸水高（浸水深を測定した場合は備考欄に入力してください．）",{"$nulls":15},"　林　豊","気象研究所地震火山研究部"]
["　　P: 港内津波高（港湾において，岸壁は越えてはいないが明確に高さが分かる津波）",{"$nulls":15},"　木村　一洋","気象研究所地震火山研究部（4/12）"]
["　　W: 微弱な津波（常時波浪との判別が不可能な微弱な津波）",{"$nulls":15},"　岩切　一宏","気象研究所地震火山研究部（4/13）"]
["*2 信頼度の判断基準"]
["　　A: 信頼度大なるもの。痕跡明瞭にして，測量誤差最も小なるもの。"]
["　　B: 信頼度中なるもの。痕跡不明につき，聞き込みにより，周囲の状況から信頼ある水位を知るもの。測量誤差小。"]
["　　C: 信頼度小なるもの。その他砂浜などで異常に波がはい上がったと思われるもの，あるいは測点が海辺より離れ測量誤差が大なるもの。"]
["　　D: 信頼度極小なるもの。高潮，台風などの影響で痕跡が重複し，不明瞭なもの，等。"]
[{"$nulls":16},"※代表者の氏名に◯を付ける．"]