Works matching DE "TELECONNECTIONS (Climatology)"
Results: 1469
Warm Arctic--cold continents: climate impacts of the newly open Arctic Sea.
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- Polar Research, 2011, v. 30, n. 1, p. 1, doi. 10.3402/polar.v30i0.15787
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An inter-comparison of six latent and sensible heat flux products over the Southern Ocean.
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- Polar Research, 2011, v. 30, n. 1, p. 1, doi. 10.3402/polar.v30i0.10167
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Decadal change in the connection between the Pacific–Japan pattern and the Indian Ocean SST basin mode.
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- Climate Dynamics, 2024, v. 62, n. 5, p. 4281, doi. 10.1007/s00382-024-07132-2
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Exploring evolutionary patterns in the teleconnections between Indian summer monsoon rainfall and Indian Ocean dipole over decades.
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- Climate Dynamics, 2024, v. 62, n. 5, p. 4041, doi. 10.1007/s00382-024-07116-2
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Effect of eastward shift of North Pacific Oscillation on the wind-evaporation-SST feedback.
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- Climate Dynamics, 2024, v. 62, n. 5, p. 3221, doi. 10.1007/s00382-023-07061-6
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The impact of boreal spring stratospheric final warming on surface air temperature over Northern Hemisphere in ERA5 and CMIP6 models.
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- Climate Dynamics, 2024, v. 62, n. 5, p. 3207, doi. 10.1007/s00382-023-07060-7
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Regional climate modeling to understand Tibetan heating remote impacts on East China precipitation.
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- Climate Dynamics, 2024, v. 62, n. 4, p. 2683, doi. 10.1007/s00382-022-06266-5
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Understanding the causes of rapidly declining prediction skill of the East Asian summer monsoon rainfall with lead time in BCC_CSM1.1m.
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- Climate Dynamics, 2024, v. 62, n. 4, p. 2807, doi. 10.1007/s00382-021-05819-4
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Assessment of seasonal forecasting errors of the ECMWF system in the eastern Indian Ocean.
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- Climate Dynamics, 2024, v. 62, n. 2, p. 1391, doi. 10.1007/s00382-023-06985-3
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Investigating bi-decadal precipitation changes over the Northwest Himalayas during the pre-monsoon: role of Pacific decadal oscillations.
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- Climate Dynamics, 2024, v. 62, n. 2, p. 1203, doi. 10.1007/s00382-023-06969-3
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Interannual teleconnections in the Sahara temperatures associated with the North Atlantic Oscillation (NAO) during boreal winter.
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- Climate Dynamics, 2024, v. 62, n. 2, p. 1123, doi. 10.1007/s00382-023-06962-w
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Interannual covariation of the thermal conditions of the southeast asian low-latitude highlands and summer East Asia–Pacific teleconnection pattern.
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- Climate Dynamics, 2024, v. 62, n. 1, p. 759, doi. 10.1007/s00382-023-06943-z
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Why is the Pacific meridional mode most pronounced in boreal spring?
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- Climate Dynamics, 2024, v. 62, n. 1, p. 459, doi. 10.1007/s00382-023-06914-4
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An investigation of the maintenance mechanisms of the quasi-biweekly Pacific-Japan teleconnection.
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- Climate Dynamics, 2024, v. 62, n. 1, p. 357, doi. 10.1007/s00382-023-06908-2
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Nonstationary modulation of the preceding spring North Pacific Victoria mode on the connection of central North America winter temperature with ENSO.
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- Climate Dynamics, 2024, v. 62, n. 1, p. 37, doi. 10.1007/s00382-023-06895-4
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Stability of ENSO teleconnections during the last millennium in CESM.
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- Climate Dynamics, 2023, v. 61, n. 11/12, p. 5699, doi. 10.1007/s00382-023-06878-5
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Using simplified linear and nonlinear models to assess ENSO-modulated MJO teleconnections.
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- Climate Dynamics, 2023, v. 61, n. 11/12, p. 5443, doi. 10.1007/s00382-023-06864-x
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Tendency-and-attention-informed deep learning for ENSO forecasts.
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- Climate Dynamics, 2023, v. 61, n. 11/12, p. 5271, doi. 10.1007/s00382-023-06854-z
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Precipitation variability using GPCC data and its relationship with atmospheric teleconnections in Northeast Brazil.
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- Climate Dynamics, 2023, v. 61, n. 11/12, p. 5035, doi. 10.1007/s00382-023-06838-z
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Skill decreases in real-time seasonal climate prediction due to decadal variability.
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- Climate Dynamics, 2023, v. 61, n. 9/10, p. 4203, doi. 10.1007/s00382-023-06800-z
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Impact of atmospheric response of ENSO and IOD on boreal summer rainfall variability over the Indian Ocean in coupled models.
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- Climate Dynamics, 2023, v. 61, n. 9/10, p. 4107, doi. 10.1007/s00382-023-06796-6
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Drivers of low-frequency Sahel precipitation variability: comparing CMIP5 and CMIP6 ensemble means with observations.
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- Climate Dynamics, 2023, v. 61, n. 9/10, p. 4449, doi. 10.1007/s00382-023-06755-1
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The weakening relationship between ENSO and the following summer Pacific Japan teleconnection since the late 1990s.
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- Climate Dynamics, 2023, v. 61, n. 7/8, p. 4033, doi. 10.1007/s00382-023-06783-x
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Contrasted influence of climate modes teleconnections to the interannual variability of coastal sea level components–implications for statistical forecasts.
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- Climate Dynamics, 2023, v. 61, n. 7/8, p. 4011, doi. 10.1007/s00382-023-06771-1
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Characterization of temperature regimes in Western Europe, as regards the summer 2022 Western European heat wave.
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- Climate Dynamics, 2023, v. 61, n. 7/8, p. 3707, doi. 10.1007/s00382-023-06760-4
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Taylor expansion of the correlation metric for an individual forecast evaluation and its application to East Asian sub-seasonal forecasts.
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- Climate Dynamics, 2023, v. 61, n. 5/6, p. 2623, doi. 10.1007/s00382-023-06702-0
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ENSO teleconnections in terms of non-NAO and NAO atmospheric variability.
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- Climate Dynamics, 2023, v. 61, n. 5/6, p. 2717, doi. 10.1007/s00382-023-06697-8
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Stage-dependent influence of PDO on interdecadal summer precipitation anomalies in eastern China.
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- Climate Dynamics, 2023, v. 61, n. 5/6, p. 2071, doi. 10.1007/s00382-023-06667-0
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ENSO teleconnections pathways in South America.
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- Climate Dynamics, 2023, v. 61, n. 3/4, p. 1277, doi. 10.1007/s00382-022-06624-3
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Mechanism of the summer rainfall interannual variability in transitional climate zone in East Asia: roles of teleconnection patterns and associated moisture processes.
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- Climate Dynamics, 2023, v. 61, n. 3/4, p. 1177, doi. 10.1007/s00382-022-06618-1
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Diverse controlling mechanisms and teleconnections of three distinctive MJO types.
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- Climate Dynamics, 2023, v. 61, n. 1/2, p. 789, doi. 10.1007/s00382-022-06604-7
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The stationarity of the ENSO teleconnection in European summer rainfall.
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- Climate Dynamics, 2023, v. 61, n. 1/2, p. 489, doi. 10.1007/s00382-022-06596-4
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The mechanism linking the variability of the Antarctic sea ice extent in the Indian Ocean sector to Indian summer monsoon rainfall.
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- Climate Dynamics, 2023, v. 60, n. 9/10, p. 2665, doi. 10.1007/s00382-022-06466-z
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The influence of the wave trains on the intraseasonal variability of the East Asian subtropical westerly jet in early and late summer.
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- Climate Dynamics, 2023, v. 60, n. 7/8, p. 2081, doi. 10.1007/s00382-022-06412-z
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The influence of Pacific-North American teleconnection on the North Pacific SST anomalies in Wintertime under the global warming.
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- Climate Dynamics, 2023, v. 60, n. 5/6, p. 1481, doi. 10.1007/s00382-022-06398-8
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Weakened relationship between ENSO and Antarctic sea ice in recent decades.
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- Climate Dynamics, 2023, v. 60, n. 5/6, p. 1313, doi. 10.1007/s00382-022-06364-4
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China.
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- Climate Dynamics, 2023, v. 60, n. 3/4, p. 981, doi. 10.1007/s00382-022-06333-x
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Atmospheric teleconnection associated with the Atlantic multidecadal variability in summer: assessment of the CESM1 model.
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- Climate Dynamics, 2023, v. 60, n. 3/4, p. 1043, doi. 10.1007/s00382-022-06331-z
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Assessing the large-scale drivers of precipitation in the northeastern United States via linear orthogonal decomposition.
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- Climate Dynamics, 2022, v. 59, n. 11/12, p. 3657, doi. 10.1007/s00382-022-06289-y
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Uncertainty in the projected changes of Sahel summer rainfall under global warming in CMIP5 and CMIP6 multi-model ensembles.
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- Climate Dynamics, 2022, v. 59, n. 11/12, p. 3579, doi. 10.1007/s00382-022-06284-3
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Three distinct convective footprints over the Indo-western Pacific that affect high temperature extreme events in Korea during boreal autumn.
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- Climate Dynamics, 2022, v. 59, n. 11/12, p. 3469, doi. 10.1007/s00382-022-06278-1
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ENSO teleconnections and atmospheric mean state in idealised simulations.
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- Climate Dynamics, 2022, v. 59, n. 11/12, p. 3287, doi. 10.1007/s00382-022-06261-w
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Understanding rainfall prediction skill over the Sahel in NMME seasonal forecast.
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- Climate Dynamics, 2022, v. 59, n. 9/10, p. 3113, doi. 10.1007/s00382-022-06263-8
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A tree ring-based hydroclimate reconstruction for eastern Europe reveals large-scale teleconnection patterns.
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- Climate Dynamics, 2022, v. 59, n. 9/10, p. 2979, doi. 10.1007/s00382-022-06255-8
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Biases and improvements of the ENSO-East Asian winter monsoon teleconnection in CMIP5 and CMIP6 models.
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- Climate Dynamics, 2022, v. 59, n. 7/8, p. 2467, doi. 10.1007/s00382-022-06220-5
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Mechanism of interannual variability of ocean bottom pressure in the South Pacific.
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- Climate Dynamics, 2022, v. 59, n. 7/8, p. 2103, doi. 10.1007/s00382-022-06198-0
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The summer Asia–North America teleconnection and its modulation by ENSO in Community Atmosphere Model, version 5 (CAM5).
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- Climate Dynamics, 2022, v. 59, n. 7/8, p. 2213, doi. 10.1007/s00382-022-06205-4
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Why is the mid-tropospheric North Atlantic subtropical high much stronger than the North Pacific subtropical high in boreal summer?
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- Climate Dynamics, 2022, v. 59, n. 5/6, p. 1883, doi. 10.1007/s00382-021-06074-3
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Long-term changes in the Arabian Peninsula rainfall and their relationship with the ENSO signals in the tropical Indo-Pacific.
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- Climate Dynamics, 2022, v. 59, n. 5/6, p. 1715, doi. 10.1007/s00382-021-06062-7
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Relationship between sea surface temperature anomalies in the Southwestern Atlantic Continental Shelf and atmospheric variability on intraseasonal timescales.
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- Climate Dynamics, 2022, v. 59, n. 5/6, p. 1539, doi. 10.1007/s00382-021-06058-3
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