標(biāo)題: Titlebook: Climatic Variations and Forcing Mechanisms of the Last 2000 Years; Philip D. Jones,Raymond S. Bradley,Jean Jouzel Conference proceedings 1 [打印本頁] 作者: 閃爍 時(shí)間: 2025-3-21 16:28
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years影響因子(影響力)
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years影響因子(影響力)學(xué)科排名
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years網(wǎng)絡(luò)公開度
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years被引頻次
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years被引頻次學(xué)科排名
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years年度引用
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years年度引用學(xué)科排名
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years讀者反饋
書目名稱Climatic Variations and Forcing Mechanisms of the Last 2000 Years讀者反饋學(xué)科排名
作者: 羊欄 時(shí)間: 2025-3-21 23:43
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作者: 使服水土 時(shí)間: 2025-3-22 03:12
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作者: intercede 時(shí)間: 2025-3-22 07:30 作者: 后天習(xí)得 時(shí)間: 2025-3-22 10:22 作者: nutrition 時(shí)間: 2025-3-22 13:33
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.作者: nutrition 時(shí)間: 2025-3-22 20:32 作者: 傲慢人 時(shí)間: 2025-3-23 00:54
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.作者: Lacunar-Stroke 時(shí)間: 2025-3-23 03:55 作者: 基因組 時(shí)間: 2025-3-23 08:13 作者: Cupping 時(shí)間: 2025-3-23 11:36 作者: 痛打 時(shí)間: 2025-3-23 16:41 作者: 太空 時(shí)間: 2025-3-23 18:59
https://doi.org/10.1007/978-3-642-61113-1Climatology; Eisbohrkerne; Global change; Globale Ver?nderung; Jahresringe; Klimatologie; Meteorologie; cor作者: 推測(cè) 時(shí)間: 2025-3-23 23:31
978-3-642-64700-0Springer-Verlag Berlin Heidelberg 1996作者: 拒絕 時(shí)間: 2025-3-24 03:23
Christian M?bius,Catherine Pallenbergrculation Models (GCMs) are becoming increasingly complex and one of the key issues in the whole ‘global warming’ debate is that of detection. When will we be able to say that we are beginning to see the changes in climate system simulated by the GCMs in observational data? Many have tried to say th作者: IST 時(shí)間: 2025-3-24 08:56 作者: saturated-fat 時(shí)間: 2025-3-24 11:27 作者: palliate 時(shí)間: 2025-3-24 15:02
Christian M?bius,Catherine Pallenberg millennial or near-millennial time scale. These records are largely derived from coniferous species at or near the elevational or latitudinal treeline across northern North America, including sites in Alaska, the Canadian Rockies, Ontario and Quebec. Although a few are based solely on living trees,作者: 昏睡中 時(shí)間: 2025-3-24 19:05 作者: reject 時(shí)間: 2025-3-25 00:47 作者: 可以任性 時(shí)間: 2025-3-25 07:19 作者: Interim 時(shí)間: 2025-3-25 08:44 作者: 藕床生厭倦 時(shí)間: 2025-3-25 14:59 作者: palette 時(shí)間: 2025-3-25 19:14 作者: 遠(yuǎn)足 時(shí)間: 2025-3-25 23:30
J. Ennker,P. Kleine,D. Pietrowskiles. Of particular interest is the linear relationship, in middle and high latitudes, between mean annual isotope concentration and mean annual temperature at the precipitation site. Paleoclimatologits have used this relationship to infer paleotemperatures from isotope paleodata, which can be extrac作者: Missile 時(shí)間: 2025-3-26 01:59 作者: 性上癮 時(shí)間: 2025-3-26 08:01
Bestandteile eines Risikomanagements, and West Antarctica may be temporally asynchronous. For example, records from the Antarctic Peninsula indicate a strong 20th century warming in which the high plateau of East Antarctica has not participated. Similarly, a recent Neoglacial cooling, the “Little Ice Age”, was prominent in East Antarct作者: 合乎習(xí)俗 時(shí)間: 2025-3-26 10:19 作者: 聲音刺耳 時(shí)間: 2025-3-26 15:31
Risikomanagement im IT-Bereich,riance is found using EOF (.mpirical .rthogonal .unctions) techniques that identify two main spatial modes that occur with nearly the same frequency. Together these two Eigenvectors explain 50% of the variance in the detrended O-18 records..One year averages of absolutely dated O-18 and precipitatio作者: irreparable 時(shí)間: 2025-3-26 19:53
Visuelle Hilfen in der Notfallmedizina. Small changes in the tropics can resonate through the climate system through their influence on regional ocean-atmosphere systems and boundary conditions. Increasingly, records from long-lived corals are being developed and applied to understand the pre-instrumental variability of the tropical oc作者: Benzodiazepines 時(shí)間: 2025-3-26 21:01 作者: 商談 時(shí)間: 2025-3-27 01:07
Christian M?bius,Catherine Pallenbergnce of long-term climate change. Other forcings may also be ‘corrupting’ the climate signal in the recent period (that used for calibrating the climate signal). Differences in the origin of the samples or changes in site ecology may also impart an inhomogeneity in the response of tree growth through作者: defray 時(shí)間: 2025-3-27 08:07 作者: 制定法律 時(shí)間: 2025-3-27 10:18
https://doi.org/10.1007/978-3-531-91944-7 and 3 . sites) that routinely cover the last 3–400 years but include millennial chronologies in all 3 species. These records show strong regional suppression in ring-width series corresponding to the early 18th century, mid-19th and late 20th century glacial events plus periods in the mid 14th, mid作者: CROW 時(shí)間: 2025-3-27 14:28
Marktcharakteristika in der Filmbranche,struction of precipitation in the Great Basin covering the period 6000 B.C. to A.D. 1979. We will use this to place in context a striking pattern of two multidecade droughts each terminated by intense wet periods in the period between A.D. 900 and 1400.作者: 半身雕像 時(shí)間: 2025-3-27 21:35
Risikomanagement in der Gefahrgutlogistikvector amplitude series derived from the first three significant principal components of tree growth with northern hemisphere 700 mb heights for spring (March-June) from 1948 to 1980. The strongest relationship discovered was between the first principal component of baldcypress growth (PC1) and spri作者: 窗簾等 時(shí)間: 2025-3-28 01:12
Risikomanagement in der Gefahrgutlogistikum analysis, we estimate the overall inter-decadal temperature signal contributed by these four oscillations and compare its recent behavior to an anomalous warming that has been in progress over Tasmania since about 1965. We find that 51% of the mean anomalous warming can be accounted for by these 作者: FLASK 時(shí)間: 2025-3-28 05:31
https://doi.org/10.1007/978-3-658-05896-8llennia in the southern Andes. A more conservative detrending than that used for developing the temperature reconstructions has been employed here to preserve the low frequency components in the tree-ring series. Maximum Entropy spectral analyses for different filter orders indicate prominent peaks 作者: concert 時(shí)間: 2025-3-28 08:34 作者: 歡呼 時(shí)間: 2025-3-28 12:46 作者: Muffle 時(shí)間: 2025-3-28 16:47 作者: arousal 時(shí)間: 2025-3-28 19:42
D. Pietrowski,J. Ennker,P. Kleinehe major periods of drought and wetness appear contemporaneous, suggesting a teleconnection for higher-frequency climatic events such as the El Ni?o-Southern Oscillation (ENSO). Now, for the first time, a longer temporal perspective is available from ice core records and it suggests that lower-frequ作者: 熱情的我 時(shí)間: 2025-3-28 23:41 作者: ensemble 時(shí)間: 2025-3-29 04:40 作者: Femish 時(shí)間: 2025-3-29 11:08
Tree-ring variables as proxy-climate indicators: Problems with low-frequency signalsnce of long-term climate change. Other forcings may also be ‘corrupting’ the climate signal in the recent period (that used for calibrating the climate signal). Differences in the origin of the samples or changes in site ecology may also impart an inhomogeneity in the response of tree growth through作者: 神圣將軍 時(shí)間: 2025-3-29 15:16 作者: 颶風(fēng) 時(shí)間: 2025-3-29 15:41
Reconciling the glacial and dendrochronological records for the last millennium in the Canadian Rock and 3 . sites) that routinely cover the last 3–400 years but include millennial chronologies in all 3 species. These records show strong regional suppression in ring-width series corresponding to the early 18th century, mid-19th and late 20th century glacial events plus periods in the mid 14th, mid作者: 停止償付 時(shí)間: 2025-3-29 23:36 作者: Allege 時(shí)間: 2025-3-30 03:40
Large-Scale Climatic Influences on Baldcypress Tree Growth Across the Southeastern United Statesvector amplitude series derived from the first three significant principal components of tree growth with northern hemisphere 700 mb heights for spring (March-June) from 1948 to 1980. The strongest relationship discovered was between the first principal component of baldcypress growth (PC1) and spri作者: Creditee 時(shí)間: 2025-3-30 04:12 作者: 長(zhǎng)處 時(shí)間: 2025-3-30 10:19 作者: 卷發(fā) 時(shí)間: 2025-3-30 14:28 作者: BRIDE 時(shí)間: 2025-3-30 17:08 作者: Antecedent 時(shí)間: 2025-3-30 23:56 作者: 有節(jié)制 時(shí)間: 2025-3-31 04:40
Climatic Changes for the last 2000 Years Inferred from Ice-Core Evidence in Tropical Ice Coreshe major periods of drought and wetness appear contemporaneous, suggesting a teleconnection for higher-frequency climatic events such as the El Ni?o-Southern Oscillation (ENSO). Now, for the first time, a longer temporal perspective is available from ice core records and it suggests that lower-frequ作者: nephritis 時(shí)間: 2025-3-31 07:56
Inter-comparison of Ice Core δ(18O) and Precipitation Records from Sites in Canada and Greenland overe sites being in phase. The second vector segregates the δ ice core sites from the met-stations..The advantage of regional stacking of ice core δ records is discussed as a means of reducing noise. The stacked records and the first influence coefficient of their first Eigenvector contain a very stro作者: 要素 時(shí)間: 2025-3-31 09:11
Coral records of climate change: understanding past variability in the tropical ocean-atmospherem Venezuela clearly monitor regional SST patterns in the tropical Atlantic. On the northern Great Barrier Reef, new data indicate that seasonally specific reconstructions of rainfall and SST can be derived from coral isotopic records. These new data join a growing body of literature supporting the d作者: Limited 時(shí)間: 2025-3-31 14:54 作者: 脖子 時(shí)間: 2025-3-31 21:34 作者: BROOK 時(shí)間: 2025-4-1 00:14
Tree-Ring Density Networks for Climate Reconstructionometric tree-ring network in the northern hemisphere north of 40° latitude. Intra-annual densities from rings as small as 30 microns can be analysed using recently improved densitometric techniques. Networks of living conifers provide densitometric data that can be calibrated against instrumental te作者: 射手座 時(shí)間: 2025-4-1 05:37 作者: 敲詐 時(shí)間: 2025-4-1 06:16 作者: innate 時(shí)間: 2025-4-1 10:47
Multimillennial dendroclimatic studies from the western United Statesle variability in pre-instrumental times. This results from the lack of ecological interaction between the widely-spaced, climate-sensitive, long-lived trees characteristic of the higher elevations of this region. The availability of climate-sensitive > 1000 year tree-ring records in the western con作者: Dorsal-Kyphosis 時(shí)間: 2025-4-1 15:14
Large-Scale Climatic Influences on Baldcypress Tree Growth Across the Southeastern United States years. Baldcypress tree-ring chronologies have been used to develop verifiable reconstructions of March through June precipitation totals representing some 50 to 70% of the instrumentally-recorded rainfall variance. These rainfall reconstructions are dominated by high interannual variability, but a
