Articles | Volume 2, issue 2
https://doi.org/10.5194/wcd-2-395-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-2-395-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Influence of ENSO on North American subseasonal surface air temperature variability
Patrick Martineau
CORRESPONDING AUTHOR
Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
Research Center for Advanced Science and Technology, The University of
Tokyo, Tokyo, Japan
Hisashi Nakamura
Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
Research Center for Advanced Science and Technology, The University of
Tokyo, Tokyo, Japan
Yu Kosaka
Research Center for Advanced Science and Technology, The University of
Tokyo, Tokyo, Japan
Related authors
Luisa E. Avilés-Podgurski, Patrick Martineau, Hua Lu, Ayako Yamamoto, Amanda C. Maycock, Andrew Orr, Tony Phillips, Thomas J. Bracegirdle, Anna E. Hogg, Grzegorz Muszynski, and Andrew Fleming
EGUsphere, https://doi.org/10.5194/egusphere-2025-6285, https://doi.org/10.5194/egusphere-2025-6285, 2026
Short summary
Short summary
Atmospheric rivers (ARs) are narrow filaments transporting vast amounts of water vapour poleward. Rarely, they reach the Arctic, driving strong warming and melt. In April 2020, two ARs reached the central Arctic within one week, raising near-surface temperatures by up to 30 °C and leading to extreme precipitation. Their distinct paths and thermodynamic evolution reveal diverse AR impacts on Arctic sea ice and precipitation extremes.
Masatomo Fujiwara, Patrick Martineau, Jonathon S. Wright, Marta Abalos, Petr Šácha, Yoshio Kawatani, Sean M. Davis, Thomas Birner, and Beatriz M. Monge-Sanz
Atmos. Chem. Phys., 24, 7873–7898, https://doi.org/10.5194/acp-24-7873-2024, https://doi.org/10.5194/acp-24-7873-2024, 2024
Short summary
Short summary
A climatology of the major variables and terms of the transformed Eulerian-mean (TEM) momentum and thermodynamic equations from four global atmospheric reanalyses is evaluated. The spread among reanalysis TEM momentum balance terms is around 10 % in Northern Hemisphere winter and up to 50 % in Southern Hemisphere winter. The largest uncertainties in the thermodynamic equation (about 50 %) are in the vertical advection, which does not show a structure consistent with the differences in heating.
Patrick Martineau, Swadhin K. Behera, Masami Nonaka, Hisashi Nakamura, and Yu Kosaka
Weather Clim. Dynam., 5, 1–15, https://doi.org/10.5194/wcd-5-1-2024, https://doi.org/10.5194/wcd-5-1-2024, 2024
Short summary
Short summary
The representation of subweekly near-surface temperature variability trends over the Southern Hemisphere landmasses is compared across multiple atmospheric reanalyses. It is found that there is generally a good agreement concerning the positive trends affecting South Africa and Australia in the spring, and South America in the summer. A more efficient generation of subweekly temperature variance by horizontal temperature fluxes contributes to the observed rise.
Ayako Yamamoto, Masami Nonaka, Patrick Martineau, Akira Yamazaki, Young-Oh Kwon, Hisashi Nakamura, and Bunmei Taguchi
Weather Clim. Dynam., 2, 819–840, https://doi.org/10.5194/wcd-2-819-2021, https://doi.org/10.5194/wcd-2-819-2021, 2021
Short summary
Short summary
While the key role of moist processes in blocking has recently been highlighted, their moisture sources remain unknown. Here, we investigate moisture sources for wintertime Euro-Atlantic blocks using a Lagrangian method. We show that the Gulf Stream, Kuroshio, and their extensions, along with the northeast of Hawaii, act as the primary moisture sources and springboards for particle ascent. We find that the evolution of the particle properties is sensitive to the moisture sources.
Andrew Orr, Hua Lu, Patrick Martineau, Edwin P. Gerber, Gareth J. Marshall, and Thomas J. Bracegirdle
Atmos. Chem. Phys., 21, 7451–7472, https://doi.org/10.5194/acp-21-7451-2021, https://doi.org/10.5194/acp-21-7451-2021, 2021
Short summary
Short summary
Reanalysis datasets combine observations and weather forecast simulations to create our best estimate of the state of the atmosphere and are important for climate monitoring. Differences in the technical details of these products mean that they may give different results. This study therefore examined how changes associated with the so-called Antarctic ozone hole are represented, which is one of the most important climate changes in recent decades, and showed that they were broadly consistent.
Luisa E. Avilés-Podgurski, Patrick Martineau, Hua Lu, Ayako Yamamoto, Amanda C. Maycock, Andrew Orr, Tony Phillips, Thomas J. Bracegirdle, Anna E. Hogg, Grzegorz Muszynski, and Andrew Fleming
EGUsphere, https://doi.org/10.5194/egusphere-2025-6285, https://doi.org/10.5194/egusphere-2025-6285, 2026
Short summary
Short summary
Atmospheric rivers (ARs) are narrow filaments transporting vast amounts of water vapour poleward. Rarely, they reach the Arctic, driving strong warming and melt. In April 2020, two ARs reached the central Arctic within one week, raising near-surface temperatures by up to 30 °C and leading to extreme precipitation. Their distinct paths and thermodynamic evolution reveal diverse AR impacts on Arctic sea ice and precipitation extremes.
Masatomo Fujiwara, Patrick Martineau, Jonathon S. Wright, Marta Abalos, Petr Šácha, Yoshio Kawatani, Sean M. Davis, Thomas Birner, and Beatriz M. Monge-Sanz
Atmos. Chem. Phys., 24, 7873–7898, https://doi.org/10.5194/acp-24-7873-2024, https://doi.org/10.5194/acp-24-7873-2024, 2024
Short summary
Short summary
A climatology of the major variables and terms of the transformed Eulerian-mean (TEM) momentum and thermodynamic equations from four global atmospheric reanalyses is evaluated. The spread among reanalysis TEM momentum balance terms is around 10 % in Northern Hemisphere winter and up to 50 % in Southern Hemisphere winter. The largest uncertainties in the thermodynamic equation (about 50 %) are in the vertical advection, which does not show a structure consistent with the differences in heating.
Patrick Martineau, Swadhin K. Behera, Masami Nonaka, Hisashi Nakamura, and Yu Kosaka
Weather Clim. Dynam., 5, 1–15, https://doi.org/10.5194/wcd-5-1-2024, https://doi.org/10.5194/wcd-5-1-2024, 2024
Short summary
Short summary
The representation of subweekly near-surface temperature variability trends over the Southern Hemisphere landmasses is compared across multiple atmospheric reanalyses. It is found that there is generally a good agreement concerning the positive trends affecting South Africa and Australia in the spring, and South America in the summer. A more efficient generation of subweekly temperature variance by horizontal temperature fluxes contributes to the observed rise.
Hideo Shiogama, Hiroaki Tatebe, Michiya Hayashi, Manabu Abe, Miki Arai, Hiroshi Koyama, Yukiko Imada, Yu Kosaka, Tomoo Ogura, and Masahiro Watanabe
Earth Syst. Dynam., 14, 1107–1124, https://doi.org/10.5194/esd-14-1107-2023, https://doi.org/10.5194/esd-14-1107-2023, 2023
Short summary
Short summary
We produced one of the largest single model initial-condition ensembles thus far using the MIROC6 coupled atmosphere–ocean global climate model (MIROC6-LE). MIROC6-LE includes historical simulations, eight single forcing historical experiments, five future scenario experiments and three single forcing future experiments with 10- or 50-ensemble members. We describe the experimental design and show initial analyses. This dataset would be useful to a wide range of research communities.
Ayako Yamamoto, Masami Nonaka, Patrick Martineau, Akira Yamazaki, Young-Oh Kwon, Hisashi Nakamura, and Bunmei Taguchi
Weather Clim. Dynam., 2, 819–840, https://doi.org/10.5194/wcd-2-819-2021, https://doi.org/10.5194/wcd-2-819-2021, 2021
Short summary
Short summary
While the key role of moist processes in blocking has recently been highlighted, their moisture sources remain unknown. Here, we investigate moisture sources for wintertime Euro-Atlantic blocks using a Lagrangian method. We show that the Gulf Stream, Kuroshio, and their extensions, along with the northeast of Hawaii, act as the primary moisture sources and springboards for particle ascent. We find that the evolution of the particle properties is sensitive to the moisture sources.
Andrew Orr, Hua Lu, Patrick Martineau, Edwin P. Gerber, Gareth J. Marshall, and Thomas J. Bracegirdle
Atmos. Chem. Phys., 21, 7451–7472, https://doi.org/10.5194/acp-21-7451-2021, https://doi.org/10.5194/acp-21-7451-2021, 2021
Short summary
Short summary
Reanalysis datasets combine observations and weather forecast simulations to create our best estimate of the state of the atmosphere and are important for climate monitoring. Differences in the technical details of these products mean that they may give different results. This study therefore examined how changes associated with the so-called Antarctic ozone hole are represented, which is one of the most important climate changes in recent decades, and showed that they were broadly consistent.
Cited articles
Alexander, M. A., Bladé, I., Newman, M., Lanzante, J. R., Lau, N.-C., and
Scott, J. D.: The Atmospheric Bridge: The Influence of ENSO Teleconnections
on Air–Sea Interaction over the Global Oceans, J. Climate, 15,
2205–2231, https://doi.org/10.1175/1520-0442(2002)015<2205:TABTIO>2.0.CO;2, 2002.
Bamston, A. G., Chelliah, M., and Goldenberg, S. B.: Documentation of a
highly ENSO-related sst region in the equatorial pacific: Research note,
Atmos.-Ocean, 35, 367–383, https://doi.org/10.1080/07055900.1997.9649597, 1997.
Barnston, A. G. and Livezey, R. E.: Classification, Seasonality and
Persistence of Low-Frequency Atmospheric Circulation Patterns, Mon. Weather
Rev., 115, 1083–1126, https://doi.org/10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2, 1987.
Barriopedro, D. and Calvo, N.: On the Relationship between ENSO,
Stratospheric Sudden Warmings, and Blocking, J. Climate, 27, 4704–4720,
https://doi.org/10.1175/JCLI-D-13-00770.1, 2014.
Bjornsson, H. and Venegas, S. A.: A Manual for EOF and SVD Analyses of
Climatic Data, Department of Atmospheric and Oceanic Sciences and Centre for
Climate and Global Change Research: McGill University, Montreal, Quebec,
1997.
Blackmon, M. L., Madden, R. A., Wallace, J. M., and Gutzler, D. S.:
Geographical Variations in the Vertical Structure of Geopotential Height
Fluctuations 1, J. Atmos. Sci., 36, 2450–2466,
https://doi.org/10.1175/1520-0469(1979)036<2450:GVITVS>2.0.CO;2,
1979.
Branstator, G.: A Striking Example of the Atmosphere's Leading Traveling
Pattern, J. Atmos. Sci., 44, 2310–2323,
https://doi.org/10.1175/1520-0469(1987)044<2310:ASEOTA>2.0.CO;2,
1987.
Bretherton, C. S., Smith, C., and Wallace, J. M.: An Intercomparison of
Methods for Finding Coupled Patterns in Climate Data, J. Climate, 5,
541–560, https://doi.org/10.1175/1520-0442(1992)005<0541:AIOMFF>2.0.CO;2, 1992.
Brunner, L., Schaller, N., Anstey, J., Sillmann, J., and Steiner, A. K.:
Dependence of Present and Future European Temperature Extremes on the
Location of Atmospheric Blocking, Geophys. Res. Lett., 45, 6311–6320,
https://doi.org/10.1029/2018GL077837, 2018.
Buehler, T., Raible, C. C., and Stocker, T. F.: The relationship of winter
season North Atlantic blocking frequencies to extreme cold or dry spells in
the ERA-40, Tellus A, 63, 212–222,
https://doi.org/10.1111/j.1600-0870.2010.00492.x, 2011.
Cai, M., Yang, S., Van Den Dool, H. M., and Kousky, V. E.: Dynamical
implications of the orientation of atmospheric eddies: A local energetics
perspective, Tellus A, 59, 127–140,
https://doi.org/10.1111/j.1600-0870.2006.00213.x, 2007.
Cattiaux, J., Vautard, R., Cassou, C., Yiou, P., Masson-Delmotte, V., and
Codron, F.: Winter 2010 in Europe: A cold extreme in a warming climate,
Geophys. Res. Lett., 37, L20704, https://doi.org/10.1029/2010GL044613, 2010.
Chen, W. Y. and Van den Dool, H. M.: Asymmetric Impact of Tropical SST
Anomalies on Atmospheric Internal Variability over the North Pacific, J.
Atmos. Sci., 54, 725–740, https://doi.org/10.1175/1520-0469(1997)054<0725:AIOTSA>2.0.CO;2, 1997.
Chen, W. Y. and Van Den Dool, H. M.: Significant change of extratropical
natural variability and potential predictability associated with the El
Niño/Southern Oscillation, Tellus A, 51,
790–802, https://doi.org/10.3402/tellusa.v51i5.14493, 1999.
Compo, G. P., Sardeshmukh, P. D., and Penland, C.: Changes of Subseasonal
Variability Associated with El Niño, J. Climate, 14, 3356–3374,
https://doi.org/10.1175/1520-0442(2001)014<3356:COSVAW>2.0.CO;2,
2001.
Di Lorenzo, E., Schneider, N., Cobb, K. M., Franks, P. J. S., Chhak, K.,
Miller, A. J., McWilliams, J. C., Bograd, S. J., Arango, H., Curchitser, E.,
Powell, T. M., and Rivière, P.: North Pacific Gyre Oscillation links
ocean climate and ecosystem change, Geophys. Res. Lett., 35, L08607,
https://doi.org/10.1029/2007GL032838, 2008.
Dole, R. M.: Persistent Anomalies of the Extratropical Northern Hemisphere
Wintertime Circulation: Structure, Mon. Weather Rev., 114, 178–207,
https://doi.org/10.1175/1520-0493(1986)114<0178:PAOTEN>2.0.CO;2,
1986.
Gollan, G. and Greatbatch, R. J.: The relationship between Northern
Hemisphere winter blocking and tropical modes of variability, J. Climate,
30, 9321–9337, https://doi.org/10.1175/JCLI-D-16-0742.1, 2017.
Hadley Centre for Climate Prediction and Research/Met Office/Ministry of Defence/United Kingdom: Hadley Centre Global Sea Ice and Sea Surface Temperature (HadISST), Research Data Archive at the National Center for Atmospheric Research, Computational and Information Systems Laboratory. https://doi.org/10.5065/XMYE-AN84, 2000.
Hinton, T. J., Hoskins, B. J., and Martin, G. M.: The influence of tropical
sea surface temperatures and precipitation on north Pacific atmospheric
blocking, Clim. Dynam., 33, 549–563, https://doi.org/10.1007/s00382-009-0542-7, 2009.
Horel, J. D. and Wallace, J. M.: Planetary-Scale Atmospheric Phenomena
Associated with the Southern Oscillation, Mon. Weather Rev., 109, 813–829,
1981.
Hsu, H.-H. and Wallace, J. M.: Vertical Structure of Wintertime
Teleconnection Patterns, J. Atmos. Sci., 42, 1693–1710,
https://doi.org/10.1175/1520-0469(1985)042<1693:VSOWTP>2.0.CO;2,
1985.
Japan Meteorological Agency: JRA-55: Japanese 55-year Reanalysis, Daily 3-Hourly and 6-Hourly Data, Research Data Archive at the National Center for Atmospheric Research, Computational and Information Systems Laboratory, https://doi.org/10.5065/D6HH6H41, 2013.
Kobayashi, S., Ota, Y., Harada, Y., Ebita, A., Moriya, M., Onoda, H., Onogi,
K., Kamahori, H., Kobayashi, C., Endo, H., Miyaoka, K., and Takahashi, K.:
The JRA-55 Reanalysis: General Specifications and Basic Characteristics, J.
Meteorol. Soc. Japan. Ser. II, 93, 5–48, https://doi.org/10.2151/jmsj.2015-001,
2015.
Kushnir, Y.: Retrograding Wintertime Low-Frequency Disturbances over the
North Pacific Ocean, J. Atmos. Sci., 44, 2727–2742,
https://doi.org/10.1175/1520-0469(1987)044<2727:RWLFDO>2.0.CO;2,
1987.
Lau, N.-C.: Interactions between Global SST Anomalies and the Midlatitude
Atmospheric Circulation, B. Am. Meteorol. Soc., 78, 21–33,
https://doi.org/10.1175/1520-0477(1997)078<0021:IBGSAA>2.0.CO;2,
1997.
Lau, N.-C. and Nath, M. J.: Variability of the Baroclinic and Barotropic
Transient Eddy Forcing Associated with Monthly Changes in the Midlatitude
Storm Tracks, J. Atmos. Sci., 48, 2589–2613,
https://doi.org/10.1175/1520-0469(1991)048<2589:VOTBAB>2.0.CO;2,
1991.
Lin, H.: Subseasonal variability of North American wintertime surface air
temperature, Clim. Dynam., 45, 1137–1155,
https://doi.org/10.1007/s00382-014-2363-6, 2015.
Lin, H. and Derome, J.: Changes in predictability associated with the PNA
pattern, Tellus A, 48, 553–571,
https://doi.org/10.3402/tellusa.v48i4.12139, 1996.
Lin, H. and Derome, J.: On the modification of the high- and low-frequency
eddies associated with the PNA anomaly: an observational study, Tellus A, 49, 87–99, https://doi.org/10.3402/tellusa.v49i1.12213,
1997.
Linkin, M. E. and Nigam, S.: The North Pacific Oscillation-West Pacific
teleconnection pattern: Mature-phase structure and winter impacts, J. Climate,
21, 1979–1997, https://doi.org/10.1175/2007JCLI2048.1, 2008.
Lorenz, E. N.: Available Potential Energy and the Maintenance of the General
Circulation, Tellus, 7, 157–167, https://doi.org/10.3402/tellusa.v7i2.8796, 1955.
Martineau, P., Chen, G., and Burrows, A. D.: Wave Events: Climatology,
Trends, and Relationship to Northern Hemisphere Winter Blocking and Weather
Extremes, J. Climate, 30, 5675–5697, https://doi.org/10.1175/JCLI-D-16-0692.1, 2017.
Martineau, P., Nakamura, H., Kosaka, Y., and Yamamoto, A.: Importance of a
vertically tilting structure for energizing the North Atlantic Oscillation,
Sci. Rep., 10, 12671, https://doi.org/10.1038/s41598-020-69551-5, 2020.
Mullen, S. L.: Model Experiments on the Impact of Pacific Sea Surface
Temperature Anomalies on Blocking Frequency, J. Climate, 2, 997–1013,
https://doi.org/10.1175/1520-0442(1989)002<0997:MEOTIO>2.0.CO;2,
1989.
Nakamura, H.: Year-to-Year and interdecadal variability in the activity of
intraseasonal fluctuations in the Northern Hemisphere wintertime
circulation, Theor. Appl. Climatol., 55, 19–32,
https://doi.org/10.1007/BF00864700, 1996.
Nishii, K., Nakamura, H., and Orsolini, Y. J.: Cooling of the wintertime
Arctic stratosphere induced by the western Pacific teleconnection pattern,
Geophys. Res. Lett., 37, L13805, https://doi.org/10.1029/2010GL043551, 2010.
Oort, A. H.: On Estimates Of The Atmospheric Energy Cycle, Mon. Weather
Rev., 92, 483–493, https://doi.org/10.1175/1520-0493(1964)092<0483:OEOTAE>2.3.CO;2, 1964.
Pfahl, S. and Wernli, H.: Quantifying the relevance of atmospheric blocking
for co-located temperature extremes in the Northern Hemisphere on
(sub-)daily time scales, Geophys. Res. Lett., 39, L12807,
https://doi.org/10.1029/2012GL052261, 2012.
Rayner, N. A., Parker, D. E., Horton, E. B., Folland, C. K., Alexander, L.
V., Rowell, D. P., Kent, E. C., and Kaplan, A.: Global analyses of sea
surface temperature, sea ice, and night marine air temperature since the
late nineteenth century, J. Geophys. Res., 108, 4407,
https://doi.org/10.1029/2002JD002670, 2003.
Renwick, J. A. and Wallace, J. M.: Relationships between North Pacific
Wintertime Blocking, El Niño, and the PNA Pattern, Mon. Weather Rev.,
124, 2071–2076, https://doi.org/10.1175/1520-0493(1996)124<2071:RBNPWB>2.0.CO;2, 1996.
Rex, D. F.: Blocking Action in the Middle Troposphere and its Effect upon
Regional Climate. I. An Aerological Study of Blocking Action, Tellus, 2,
196–211, https://doi.org/10.1111/j.2153-3490.1950.tb00331.x, 1950.
Sheng, J.: GCM experiments on changes in atmospheric predictability
associated with the PNA pattern and tropical SST anomalies, Tellus A, 54, 317–329, https://doi.org/10.3402/tellusa.v54i4.12153, 2002.
Sheng, J. and Derome, J.: An observational study of the energy transfer
between the seasonal mean flow and transient eddies, Tellus A, 43,
128–144, https://doi.org/10.1034/j.1600-0870.1991.t01-1-00004.x, 1991.
Sillmann, J., Mischa, C. M., Kallache, M., and Katz, R. W.: Extreme cold
winter temperatures in Europe under the influence of North Atlantic
atmospheric blocking, J. Climate, 24, 5899–5913,
https://doi.org/10.1175/2011JCLI4075.1, 2011.
Simmons, A. J., Wallace, J. M., and Branstator, G. W.: Barotropic Wave
Propagation and Instability, and Atmospheric Teleconnection Patterns, J.
Atmos. Sci., 40, 1363–1392, https://doi.org/10.1175/1520-0469(1983)040<1363:BWPAIA>2.0.CO;2, 1983.
Smith, C. A. and Sardeshmukh, P. D.: The effect of ENSO on the intraseasonal
variance of surface temperatures in winter, Int. J. Climatol., 20,
1543–1557, https://doi.org/10.1002/1097-0088(20001115)20:13<1543::AID-JOC579>3.0.CO;2-A, 2000.
Soulard, N., Lin, H., and Yu, B.: The changing relationship between ENSO and
its extratropical response patterns, Sci. Rep., 9, 6507,
https://doi.org/10.1038/s41598-019-42922-3, 2019.
Straus, D. M. and Shukla, J.: Does ENSO Force the PNA?, J. Climate, 15,
2340–2358, 2002.
Sung, M.-K., Jang, H.-Y., Kim, B.-M., Yeh, S.-W., Choi, Y.-S., and Yoo, C.:
Tropical influence on the North Pacific Oscillation drives winter extremes
in North America, Nat. Clim. Change, 9, 413–418,
https://doi.org/10.1038/s41558-019-0461-5, 2019.
Taguchi, S. and Asai, T.: Statistical Characteristics of Long-Lived
Large-Scale Disturbances in the Northern Hemisphere 500hPa Height Fields, J.
Meteorol. Soc. Japan. Ser. II, 65, 221–236,
https://doi.org/10.2151/jmsj1965.65.2_221, 1987.
Takaya, K. and Nakamura, H.: A formulation of a wave-activity flux for
stationary Rossby waves on a zonally varying basic flow, Geophys. Res.
Lett., 24, 2985–2988, https://doi.org/10.1029/97GL03094, 1997.
Takaya, K. and Nakamura, H.: A Formulation of a Phase-Independent
Wave-Activity Flux for Stationary and Migratory Quasigeostrophic Eddies on a
Zonally Varying Basic Flow, J. Atmos. Sci., 58, 608–627,
https://doi.org/10.1175/1520-0469(2001)058<0608:AFOAPI>2.0.CO;2,
2001.
Takaya, K. and Nakamura, H.: Geographical dependence of upper-level blocking
formation associated with intraseasonal amplification of the Siberian high,
J. Atmos. Sci., 62, 4441–4449, https://doi.org/10.1175/JAS3628.1, 2005.
Tam, C. Y. and Lau, N. C.: The impact of ENSO on atmospheric intraseasonal
variability as inferred from observations and GCM simulations, J. Climate,
18, 1902–1924, https://doi.org/10.1175/JCLI3399.1, 2005.
Tanaka, S., Nishii, K., and Nakamura, H.: Vertical structure and energetics
of the Western Pacific teleconnection pattern, J. Climate, 29, 6597–6616,
https://doi.org/10.1175/JCLI-D-15-0549.1, 2016.
Trenberth, K. E., Branstator, G. W., Karoly, D., Kumar, a, Lau, N. C., and
Ropelewski, C.: Progress during TOGA in understanding and modeling global
teleconnections associated with tropical sea surface temperatures, J.
Geophys. Res., 103, 14291–14324, https://doi.org/10.1029/97jc01444, 1998.
Wallace, J. M. and Gutzler, D. S.: Teleconnections in the Geopotential
Height Field during the Northern Hemisphere Winter, Mon. Weather Rev.,
109, 784–812, https://doi.org/10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;2, 1981.
Wilks, D. S.: The Stippling Shows Statistically Significant Grid Points,
B. Am. Meteorol. Soc., 97, 2263–2274, 2016.
Short summary
To better understand the factors that impact the weather in North America, this study explores the influence of the El Niño–Southern Oscillation on wintertime surface air temperature variability using reanalysis data. Results show that La Niña enhances subseasonal variability over western North America by amplifying the baroclinic conversion of energy from the winter-mean circulation to subseasonal eddies. Changes in the structural properties of eddies are crucial for this amplification.
To better understand the factors that impact the weather in North America, this study explores...