Titlebook: Climatic Variations and Forcing Mechanisms of the Last 2000 Years; Philip D. Jones,Raymond S. Bradley,Jean Jouzel Conference proceedings 1

只看該作者 · 發(fā)表于 2025-3-21 16:28:14

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years影響因子(影響力)

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years影響因子(影響力)學(xué)科排名

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years網(wǎng)絡(luò)公開(kāi)度

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years網(wǎng)絡(luò)公開(kāi)度學(xué)科排名

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years被引頻次

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years被引頻次學(xué)科排名

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years年度引用

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years年度引用學(xué)科排名

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years讀者反饋

書(shū)目名稱(chēng)Climatic Variations and Forcing Mechanisms of the Last 2000 Years讀者反饋學(xué)科排名

只看該作者 · 發(fā)表于 2025-3-21 23:43:32

Conference proceedings 1996levance to the next century and that for which there is the most evidence. High-resolution proxy records for this period are available from a variety of sources. Five sections consider dendroclimatology, ice cores, corals, historical records, lake varves, and other indicators. The final two sections

只看該作者 · 發(fā)表于 2025-3-22 03:12:59

1431-7125 of most relevance to the next century and that for which there is the most evidence. High-resolution proxy records for this period are available from a variety of sources. Five sections consider dendroclimatology, ice cores, corals, historical records, lake varves, and other indicators. The final tw

只看該作者 · 發(fā)表于 2025-3-22 07:30:56

只看該作者 · 發(fā)表于 2025-3-22 10:22:56

只看該作者 · 發(fā)表于 2025-3-22 13:33:31

Christian M?bius,Catherine Pallenbergtion on how or if certain climatic features of the past millennium (the Medieval Warm Epoch and Little Ice Age) were manifested in the northern Americas; Canada and the U. S. state of Alaska. These data are also valuable for determining how such natural fluctuations compare to recent, possibly anthropogenic climatic change.

只看該作者 · 發(fā)表于 2025-3-22 20:32:30

只看該作者 · 發(fā)表于 2025-3-23 00:54:47

Introductionuctuations and cycles have occurred on longer timescales. We live in an interglacial climate, a warm phase on the 10,000 year timescale, in a period known as the Quaternary, dominated for the most part by Ice Age Climates.

只看該作者 · 發(fā)表于 2025-3-23 03:55:50

只看該作者 · 發(fā)表于 2025-3-23 08:13:30

		自動(dòng)登錄	找回密碼
密碼			To register

關(guān)于派博傳思			派博傳思旗下網(wǎng)站			友情鏈接
派博傳思介紹	公司地理位置	論文服務(wù)流程	影響因子官網(wǎng)	吾愛(ài)論文網(wǎng)	大講堂	北京大學(xué)	Oxford Uni.	Harvard Uni.
發(fā)展歷史沿革	期刊點(diǎn)評(píng)	投稿經(jīng)驗(yàn)總結(jié)	SCIENCEGARD	IMPACTFACTOR	派博系數(shù)	清華大學(xué)	Yale Uni.	Stanford Uni.
\|Archiver\|手機(jī)版\|小黑屋\| 派博傳思國(guó)際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-18 21:30
Copyright © 2001-2015 派博傳思京公網(wǎng)安備110108008328 版權(quán)所有 All rights reserved