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【バーチャルYouTuber】.LIVEアイドル部ファンスレ#4932【アップランド】
レス数が1000を超えています。これ以上書き込みはできません。
0001名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:38:45.30
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※前スレ
【バーチャルYouTuber】.LIVEアイドル部ファンスレ#4930【アップランド】
https://egg.5ch.net/test/read.cgi/streaming/1599455333/
https://twitter.com/5chan_nel (5ch newer account)
【バーチャルYouTuber】.LIVEアイドル部ファンスレ#4931【アップランド】
https://egg.5ch.net/test/read.cgi/streaming/1599473442/
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https://twitter.com/5chan_nel (5ch newer account)
0016名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:40:19.75
おしゅしアイス😊
0031名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:41:23.89
これを解読してくれ

448 名無しさん＠お腹いっぱい。 (ｽﾌﾟｯｯ Sd03-D7hh [1.75.208.61]) [sage] 2020/09/07(月) 20:34:48.43 ID:JH9ZHZEid
>>430
これな、相手はドル部ドル信じゃなくてア信
これをうまく取り除けばV界隈をクリーンにしつつドル部も健全化塩も安心して活動できる
0033名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:41:29.10
ドル部の悪くないお話は未だにトラウマなんだよ
0049名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:42:54.81
>>24
めめめの顔でいつも吹いてまうわ😅
0050名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:42:56.36
怖くはないけど楽しみでもない

怖い
0058名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:44:02.01
>>51
わかる
友達と少額賭けてやったらめちゃくちゃ盛り上がりそう
0072名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:45:21.88
拗ねてるふーちゃんクソかわいくない？
0077名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:45:41.95
メンシについてとかか？
0096名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:46:57.13
お話っても他のメンバーの話はしないだろ😅
0113名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:47:49.98
【速報】ふーちゃん、ゴースティングに激怒
0122名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:48:28.15
ふーちゃんかわいい
0127名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:48:49.13
因幡はねる「情報流してやる！5chに書きこみまくってやる！」
犬山たまき「やめろ5chに書くの！開示しますよ！開示！」
因幡はねる「noteやってないから大丈夫だもんね～」
0134名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:49:22.70
>>104　
ドル部で検索してるので大丈夫ですわ🤗大丈夫ですわ🤗
0143名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:50:13.72
>>113
このゲームゴースティング関係ない...
0162名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:51:26.42
前に平井の曲のめめめＭＡＤや、電撃棒でbadappleＭＡＤ作ってた人が新作めめめに速攻ＲＴくらってリプもらってる
よかったな
0185名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:53:01.37
ふーさんの遊び大全普通にどれも面白いんだ��
個人的には花札してる時のクレバーなふーさんがすこだったからもっとやって欲しいんだ��
0193名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:53:26.70
なとりはまだアイドル部やろ
なとりで対立煽りするなら他にドルアンとドルファンの違い教えてくれや
0207名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:53:57.31
>>168
まぁ映画見るだけだからなぁ
0229名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:54:40.02
すず以上に下手くそで笑う
0234名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:54:51.03
>>31
IP用語解説

・ドル部:アイドル部のこと

・ドル信:アイドル部のことが好きな人
一般的に健常、普通のリスナーのことを指す

・ア信:アップランド信者のこと
アップランドageのためならアイドル部さえ攻撃するガイジ、厄介、馬組のことを指す
※類語:アシン

IPスレではドル信、ア信は使い分け、ドル信は攻撃するな、ア信だけ晒せとする風潮がある
0289名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:57:47.99
ふーちゃん膣連呼してます……
0302名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:58:25.10
ガーイ……
0303名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 20:58:25.06
なんのこだわりか知らんけど
>>1のツイッターまとめを夜桜たまのリストに直す奴がいるんだわ
ほんと迷惑なんでやめてくれ
0346名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:00:15.84
>>1
>>950
次スレ本文これで立てて


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!extend:none:none:BLS:512
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・スレを立てるときは先頭に
「!extend:none:none:BLS:512」を三行いれよう
─────────────────────────────────────────────
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※前スレ
【バーチャルYouTuber】.LIVEアイドル部ファンスレ#4932【アップランド】
https://egg.5ch.net/test/read.cgi/streaming/1599478725/
https://twitter.com/5chan_nel (5ch newer account)
0354名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:00:42.01
めめめ今日いつもより可愛くないか？
0358名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:00:56.55
すまん、ふーちゃんガイジ扱いするのやめていいか？
かわいすぎるわ
0361名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:01:24.38
予定が言える
案件に被せない気遣い
一旦区切ってからスパチャ読み

すまん、双葉って”健常”なのでは？
0377名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:02:20.06
はい初手めめごん
0389名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:02:54.40
イオリ〜😭明日のおはなし怖いよ〜😭
0410名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:03:33.54
さぁ次の同時視聴はだれだ
0419名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:04:04.75
この後すずぺくすやるかもです
0421名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:04:08.15
花京院ちえり🍒@chieri_kakyoin32秒
青鬼！！！！
映画観るの初めて(((* ॑꒳ ॑* ≡ * ॑꒳ ॑* )))ｿﾜｿﾜ
ぶるーべりぃ〜

ちえりママも病室から見てます
0429名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:04:23.79
ちゃんとテーマトークできるだと...!?
0440名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:04:39.77
>>80
そらは顔から下がバランス悪いしテクスチャが手抜きなのがな
そもそも上半身の静止画だけで比較するのは間違ってるし
0442名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:04:47.17
>>427
案件に決まってんだろ
0471名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:05:46.17
おしゅし😈

🍣🍣🍣　🍣　 　　🍣 　🍣　🍣
🍣　 　 　 🍣　 　🍣 　　🍣　🍣
🍣🍣🍣　　🍣　🍣 　 　🍣　🍣
🍣 　 　 　 　 🍣🍣　　 　🍣　🍣 　 　 　 🍣🍣
🍣🍣🍣　　 　🍣 　 　 　🍣　🍣🍣🍣　 🍣🍣
0473名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:06:00.78
同時視聴ってツッコミどころ多いぐらいの方が良くない？
0475名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:06:09.59
ニコニコは1月ぐらいにドルタグひどすぎて解約したけどなぜか最近洗浄されたからプレミアム再登録したわ
0514名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:08:19.39
>>473
めめめが昔見たババアが無双するホラー映画は配信としてて楽しかったし絶対一人ではクソ映画だったからいいチョイスだった
0527名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:09:11.27
>>498
これ
普通に面白い作品は普通に1人で見たいんや
0545名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:09:57.86
>>512
実際フリゲー出始めた時は今までのホラゲーで1番怖かったて言えるくらい怖かった
フリゲー特有のRPGツクール調の雰囲気も怖さに拍車をかけてた
0548名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:10:09.57
対立煽りするのって最高にオタクって感じで好き
0570名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:11:34.82
スレ番引き継いどいて完全にまっさら状態から始められるわけねーだろ
ドルアンに生きていたことの罪は転生しない限り消えねぇんだよ！
0587名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:12:43.13
ちえりはそろそろメジャーどころのゲームを挟め
0628名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:14:51.26
>>604
ちぇりーぱいの間🤗
0636名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:15:03.13
罪を全部IPに押し付けることで上手くやってたのがファンスレアンスレの対立構造になって内部で煽り合ってるのアホすぎるでしょ
狙ってやってるなら結構賢いけど
0648名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:15:38.82
塩害が普段より暴れてるけど塩関連でなんかあった？
0658名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:16:01.41
IPランドさぁ…塩餡にいじめられて敗北したからってドルファン荒らしに来るのやめな
最高にダサいぞ
0662名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:16:15.07
>>544
お仕事を回さなければならないから
なんの意味もないようなもんだけど給料を与えるためだけに存在する仕事がこの世にはごまんとあるだろ？
0676名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:16:53.92
>>640
そもそもいろはが初手に宣伝したのが...
0682名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:17:14.67
>>659
もちもコラボ。🐑
のめめめが懐かしいんだ😭
0710名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:18:21.13
>>640
こういうのって普通は最後の方に宣伝しない？
0721名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:19:03.69
>>648
まいてつってイベントを塩が辞退したってさ
それでIPガイジが塩餡にキレてる
そのカウンターが今無しスレに来てる

875 名無しさん＠お腹いっぱい。 (ｱｳｱｳｸｰ MM01-T5IU [36.11.228.154]) sage 2020/09/07(月) 19:25:57.99 ID:VSmIGLyqM
塩餡が好き放題やってる状況がそろそろ本気で悔しくなってきたからカウンターしていいか？
0754名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:20:15.48
塩餡はいいよな、どれだけ暴れてもカウンターはこっちにくるんだもん
塩信は北朝鮮と戦争になったら日本に攻めてくる韓国人かよ
0778名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:21:15.86
>>752
はねるはガチ たまきは知らん
0814名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:22:52.72
　　　　／V＼
　　　　/◎;;;,;,,,,ヽ
　＿　ﾑ::::( 😆　)| おしゅしの新衣装‼
ヽﾂ.（ﾉ::::::::::.:::::.:..|）
　 ヾソ:::::::::::::::::.:ﾉ
　　 ｀ ー U'"U'
0870名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:25:46.42
MaThe chapterksma has described z, the measurementms,s, system and ma,the procedure followed for the computationjsm of the fluxes and the msmprocedure of flux summation,x,s, including
data gap filling strategy, night msmtflux corrections and error estimationmdke. It begins with the introduction of estimates of themz, annual net carbongw, and water exchange maof forests using the EUROFLUX methodology. The chapter then provides us with the theory and x,moves on to discuss the eddy covariance system and its sonic anemometer, temperature,a,a x fluctuation zlal measurementsm
,, infrared gas analyser, air
transport system, and tower instrumentation. Additional measurements are also given in the chapter. Data acquisition and its computation,a, and correction is discussedmxk next in the chapter by giving its general procedurejd , half-hourly means (malco-)variances and uncorrected fluxes,
0872名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:25:55.69
塩くん！？
0884名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:26:18.82
The chapter hasnsm ksks
described the measurementjfjx system and the procedure followed for the computation of the fluxes and the proceduremcme of ickdflux summation, including data gap filling strategy,
Mdmnight flux corrections and error estimation. It begins with the introductionjxjs of estimates of the annual net carbon and water exchange of forests using the hshei methodology. The chapter then provides us with the theory and moves on to
discuss the eddy covariance
system and its sonic anemometer, temperature fluctuationj measurements, infrared gas jsjsj, air transport system, and tower instrumentation. Additional measurements are also given in the chapter. NsData acquisition and its computation and
correction is discussed jdmejnext in the chapter by giving its general procedure, half-hourly means (co-)variances and uncorrected fluxes,
0894名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:26:56.89
providesnzj us with the theory andmzm moves on to discuss the eddy covariance system and its sonic anemometer, temperature fluctuation measurementsmzm, infrared gas analyser, air transport system, and tower instrumentation. Additional measurementskjsjs are also given in the chapter. Data acquisition and its computation and correction is discussed next in the chapter by giving its general procedure, nanshalf-hourly hhanmeans (co-)variances and uncorrected fluxes, intercomparison of software, and correction for frequency response losses. The chapter has also discussed about quality control and nansfour criteria are investigated here for the same. Spatial representativeness of measured fluxes and summation procedure are reviewed. The chapter then moves on to the discussion of data gap filling through interpolation and parameterization and neural networks. Corrections to night-time data and error estimation are also mwjexplored in the chapter. Finally, the chapter closes with conclusionsha.

Previous chapterNext chapter
Copyright © 2000 Academic Press. Published by Elsevier Ltd. All rights reserved.

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0905名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:27:19.78
Mzjsmwm us with the theory andmzm moves on to discuss the eddy covariance system and its sonic anemometer, temperature fluctuation measurementsmzm, infrared gas analyser, air transport system, and tower instrumentation. Additional measurementskjsjs are also given in the chapter. Data acquisition and its computation and correction is discussed next in the chapter by giving its general procedure, nanshalf-hourly hhanmeans (co-)variances and uncorrected fluxes, intercomparison of software, and correction for frequency response losses. The chapter has also discussed about quality control and nansfour criteria are investigated here in aysnfor the same. Spatial representativeness of measured fluxes and summation procedure are reviewed. The chapter then moves on to the discussion of data gap filling through interpolation and jsjsj and neural networks. Corrections to night-time data and error estimation are also mwjexplored in the chapter. Finally, the chapter closes with conclusionsha.

Previous chapterNext chapter
Copyright © 2000 Academic Press. Published by Elsevier Ltd. All rights reserved.

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Agricultural and Forest Meteorology, Volume 156, 2012, pp. 65-74
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Combining eddy-covariance and chamber measurements to determine the methane budget from a small, heterogeneous urban floodplain wetland park

and Forest Meteorology, Volumes 237–238, 2017, pp. 160-170
Purchase PDFView details
Combining stable isotopes, Eddy Covariance system and meteorological measurements for partitioning evapotranspiration, of winter wheat, into soil evaporation and plant transpiration in a semi-arid region
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Citationsjajw
Citation Indexes: 1415
Patent Family Citations: 1
Captures
Readers: 624
0907名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:27:38.21
providesnzj us with the theory andmzm moves on to discuss the eddy covariance system and its sonic anemometer, jsmsm fluctuation measurementsmzm, infrared gas analyser, air transport system, and tower instrumentation. Additional measurementskjsjs are also given in the chapter. Data acquisition and its computation and correction is discussed next in the chapter by giving its general procedure, nanshalf-hourly hhanmeans (co-)variances and uncorrected fluxes, jxjej of software, and correction for frequency response msmslosses. The chapter has also discussed about quality control and nansfour criteria are investigated here jsmsm the same. Spatial representativeness of measured fluxes and summation procedure are reviewed. The chapter then moves on to the discussion of data gap filling through interpolation and parameterization and neural networks. Corrections to night-time data and error estimation are also mwjexplored in the chapter. Finally, the chapter closes with conclusionsha.

Previous nzmajschapterNext chapter
Copyright © 2000 Academic Press. Published by Elsevier Ltd. All rights reserved.

Recommended articles
Reflections on the surface energy imbalance problem
Agricultural and Forest Meteorology, Volume 156, 2012, pp. 65-74
Purchase PDFView details
Combining eddy-covariance and chamber measurements to determine the methane budget from a small, heterogeneous urban floodplain wetland park

and Forest Meteorology, Volumes 237–238, 2017, pp. 160-170
Purchase PDFView details
Combining stable isotopes, Eddy Covariance system and meteorological measurements for partitioning evapotranspiration, of winter wheat, into soil evaporation and plant transpiration in a semi-arid region
Agricultural Water Management, Volume 177, 2016, pp. 181-192
Purchase PDFView details
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Citing articles (1415)

Article Metrics
Citations
Citation Indexes: 1415
Patent Family Citations: 1
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Readers: 624
0915名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:27:58.03
E MaThe chapterksma has described z, the measurementms,s, system and ma,the procedure followed for the computationjsm of the fluxes and the msmprocedure of flux summation,x,s, including
data gap filling strategy, night msmtflux corrections and error estimationmdke. It begins with the introduction of estimates of themz, annual net carbongw, and water exchange maof forests using the EUROFLUX methodology. The chapter then provides us with the theory and x,moves on to discuss the eddy covariance system and its sonic anemometer, temperature,a,a x fluctuation zlal measurementsm
,, infrared gas analyser, air
transport system, and tower instrumentation. Additional measurements are also given in the chapter. Data acquisition and its computation,a, and correction is discussedmxk next in the chapter by giving its general procedurejd , half-hourly means (malco-)variances and uncorrected fluxes,w

MaThe chapterksma has described z, the measurementms,s, system and ma,the procedure followed for the computationjsm of the fluxes and the msmprocedure of flux summation,x,s, including
data gap filling strategy, night msmtflux corrections and error estimationmdke. It begins with the introduction of estimates of themz, annual net carbongw, and water exchange maof forests using the EUROFLUX methodology. The chapter then provides us with the theory and x,moves on to discuss the eddy covariance system and its sonic anemometer, temperature,a,a x fluctuation zlal measurementsm
,, infrared gas analyser, air
transport system, and tower instrumentation. Additional measurements are also given in the chapter. Data acquisition and its computation,a, and correction is discussedmxk next in the chapter by giving its general procedurejd , half-hourly means (malco-)variances and uncorrected fluxes,
0921名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:28:15.63
MaThe




has described z, the measurementms,s, system and ma,the procedure followed for the computationjsm of the fluxes and the msmprocedure of flux summation,x,s, including
data

filling strategy, night msmtflux corrections and error estimationmdke. It begins with the introduction of estimates of themz, annual net carbongw, and water exchange maof forests using the EUROFLUX methodology. The chapter then provides us with the theory and x,moves on to discuss the eddy covariance system and its sonic anemometer, temperature,a,a x fluctuation zlal measurementsm
,, infrared gas


analyser, air
transport system, and tower instrumentation. Additional measurements are also given in the chapter. Data acquisition and its computation,a, and correction is discussedmxk next in the chapter by giving its general procedurejd , half-hourly means (malco-)variances and uncorrected fluxes,
0926名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:28:26.89
providesnzj us with the theory andmzm moves on to discuss the eddy covariance system and its sonic anemometer, jsmsm fluctuation measurementsmzm, infrared gas analyser, air transport system, and tower instrumentation. Additional measurementskjsjs are also given in the chapter. Data acquisition and its computation and correction is discussed next in the chapter by giving its general procedure, nanshalf-hourly hhanmeans (co-)variances and uncorrected fluxes, jxjej of software, and correction for frequency response msmslosses. The chapter has also discussed about quality control and nansfour criteria are investigated here jsmsm the same. Spatial representativeness of measured fluxes and summation procedure are reviewed. The chapter then moves on to the discussion of data gap filling through interpolation and parameterization and neural networks. Corrections to night-time data and error estimation are also mwjexplored in the chapter. Finally, the chapter closes with conclusionsha.

Previous nzmajschapterNext chapter
Copyright © 2000 Academic Press. Published by Elsevier Ltd. All rights reserved.

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0936名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:29:01.40
Carbon exchange between
the terrestrial biosphere and the atmosphere is one of the key processes that need to be assessed in the context of the Kyoto Protocol1
. Several studies suggest that the terrestrial biosphere is gaining carbon2,3,4,5,6,7,8, but these estimates are obtained primarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
0937名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:29:06.55
ホモビっぽいな
0945名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:29:27.79
Carbon exchange between
the terrestrial biosphere and the atmosphere is one of the key processes that need to be assessed in the context of the Kyoto Protocol1

. Several studies suggest that the terrestrial biosphere is gaining carbon2,3,4,5,6,7,8, but these estimates are obtained hahaiwkprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that
many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes haha
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data showmamsmw a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
0956名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:29:48.76
from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
0961名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:30:04.27
from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net usjw
ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
0965名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:30:15.18
from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
0972名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:30:44.50
BACKGROUND
Sentinel-lymph-node biopsy is associated with increased melanoma
-specific survival (i.e., survival until death from melanoma) among patients with node-positive intermediate-thickness
melanomas (1.2 to 3.5 mm). The value of completion lymph-node dissection for patients with sentinel-node metastases is not

METHODS
In an international trial, we randomly assigned patients with sentinel-node metastases detected by means of standard pathological assessment or a multimarker molecular assay to immediate completion lymph-node dissection (dissection group) or nodal observation with ultrasonography (observation group). The
primary end point was melanoma-specific survival. Secondary end points included disease-free survival and the cumulative rate of nonsentinel-node metastasis.
0978名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:31:15.88
RESULTS
Immediate completion
lymph-node dissection was not associated with increased melanoma-specific survival among 1934 patients with data that
could be evaluated
in an intention-to-treat analysis or
among 1755 patients in the per-protocol analysis. In the per-protocol analysis, the
mean (±SE) 3-year rate of melanoma
-specific survival was similar in the dissection group and the observation
group (86±1.3% and
86±1.2%, respectively; P=0.42 by the log-rank test) at a median follow-up of 43 months. The rate of disease-free
survival
was slightly higher
in the dissection group than in the observation group (68±1.7% and 63±1.7%, respectively; P=0.05 by the log-rank test) at 3 years, based on an increased rate of disease control in the regional nodes at 3 years (92±1.0% vs.
77±1.5%; P<0.001 by the log-rank test); these results must be interpreted with caution. Nonsentinel-node metastases, identified
in 11.5% of the patients in the
dissection group, were a strong, independent
prognostic factor for recurrence (hazard ratio, 1.78; P=0.005). Lymphedema was observed in 24.1% of the patients in the dissection group and in 6.3% of
those in the observation group.
0983名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:31:39.96
Sentinel-lymph-node
biopsy is a standard procedure
in the care of appropriately selected patients with melanoma. The first Multicenter Selective Lymphadenectomy Trial (MSLT-I) confirmed
the value of early nodal evaluation and treatment.1-3 This
prospective, international, randomized trial showed that the pathologic status of the sentinel node or nodes was the most important prognostic factor and that patients who underwent sentinel-node biopsy had fewer recurrences of melanoma than patients who underwent
wide excision and nodal
observation. Among patients with intermediate-thickness melanomas (defined as 1.2 to 3.5 mm) and nodal metastases, early surgical
treatment, guided by sentinel-node biopsy, was associated with increased melanoma-specific survival (survival until death from melanoma). These results provide support for the recommendation by several professional organizations that staging by means of sentinel-node biopsy
should be performed when appropriate.4-7
0984名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:31:44.31
>>974
🥶🔪
0990名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:32:03.70
Currently,
immediate completion lymph
-node dissection (removal of the remaining regional lymph nodes after sentinel-node excision) is usually recommended
for patients with sentinel-node metastases. However, prospective evidence
of the efficacy of
completion lymph-node dissection is lacking, and the procedure carries a risk of adverse events.8 Results of retrospective evaluations
of the
usefulness of completion
lymph-node dissection are inconclusive
.9-11 Available data from one prospective study do not suggest a benefit from immediate
dissection, but this study is not sufficiently powered
to rule out a clinically significant benefit
.12 In addition
, in most patients,
nodal disease
is limited to the sentinel lymph node or nodes and is removed by means of biopsy. Conversely, patients with even microscopic
involvement of nonsentinel nodes have an overall poorer prognosis and outcomes that are similar to those in patients
with clinically apparent
nodal disease.13,14
0997名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:32:17.78
from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
0999名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:32:23.66
from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
1000名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:32:26.04
おしゅし😊
1003名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:32:31.75
from an uptake of 6.6 tonnes of
carbon per hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems usjsto be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net

ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate. Here we present data of net ecosystem carbon exchange
, collected between 1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
1007名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:32:46.80
from an
uptake of 6.6 tonnes of
carbon
per hectarenamma per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem

carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensingnsnw of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate.

Here we present data of net ecosystem carbon exchange
, collected between
1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas
the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
1012名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:33:11.95
from an
uptake of 6.6 tonnes of
carbon
per hectarenamma per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem

carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensingnsnw of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate.

Here we present data of net ecosystem carbon exchange
, collected between
1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas
the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
1017名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:33:30.18
Ns,s,ethat, in general, ecosystem respiration determines
net
ecosystem

carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensingnsnw of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate.

Here we present data of net ecosystem carbon exchange
, collected between
1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas
the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
1018名無しさん＠お腹いっぱい。
垢版 |
2020/09/07(月) 21:33:45.72
Kaks, an
uptake of 6.6 tonnes of
carbon
per hectarenamma per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data ka a significant increase of carbon uptake with decreasing
latitude, whereas the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net
ecosystem

carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensingnsnw of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient. Uprimarily by indirect
methods, and the factors that control terrestrial carbon exchange, its magnitude and primary locations, are under debate.

Here wmapresent data of net ecosystem carbon exchange
, collected between
1996 and 1998 from
15 European forests, which confirm that many European forest ecosystems act as carbon sinks. The annual carbon balances range from an uptake of 6.6 tonnes of
carbon ksms

hectare per year to a release of nearly 1 t C ha-1 yr-1, with a large variability between forests. The data show a significant increase of carbon uptake with decreasing
latitude, whereas
the gross primary production seems to be largely independent of latitude. Our observations indicate that, in general, ecosystem respiration determines
net ecosystem
carbon exchange. Also, for an accurate assessment of the carbon balance in a particular forest ecosystem, remote sensing of the normalized difference
vegetation index or estimates based on forest inventories may not be sufficient.
10191019
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Over 1000Thread
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