{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,30]],"date-time":"2025-10-30T22:38:42Z","timestamp":1761863922343,"version":"build-2065373602"},"reference-count":12,"publisher":"MDPI AG","issue":"1","license":[{"start":{"date-parts":[[2018,12,26]],"date-time":"2018-12-26T00:00:00Z","timestamp":1545782400000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/100006961","name":"California Institute of Technology","doi-asserted-by":"publisher","award":["1460339"],"award-info":[{"award-number":["1460339"]}],"id":[{"id":"10.13039\/100006961","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Cloud-top height is an important climate variable due to its greenhouse effect, as well as being a useful indicator of circulation patterns. We use effective height anomalies from stereo retrievals at a horizontal resolution of 1.1 km after subtracting regional and seasonal mean values. After 18 years, any trend in the global average height anomaly remains hidden by the stronger influence of intermittent El Ni\u00f1o\u2013Southern Oscillation (ENSO) events. However, interesting teleconnections and oscillatory patterns in regional cloud heights are starting to emerge. Different teleconnection patterns are now evident during the El Ni\u00f1o and La Ni\u00f1a phases giving rise to high values of the correlation coefficient between many global regions and the Central Pacific, which shows the greatest connection to ENSO. Cloud heights over the Central Pacific and Maritime Continent oscillate out of phase with each other and have nearly synchronous zero anomalies with a mean separation of about 1.8 years. These are lagged by one month from similar zero values in the Southern Oscillation Index. Surface zonal wind anomalies for these two regions also oscillate out of phase with each other, and are highly correlated with the height anomalies, leading them by one month.<\/jats:p>","DOI":"10.3390\/rs11010032","type":"journal-article","created":{"date-parts":[[2018,12,26]],"date-time":"2018-12-26T11:31:21Z","timestamp":1545823881000},"page":"32","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":3,"title":["ENSO and Teleconnections Observed Using MISR Cloud Height Anomalies"],"prefix":"10.3390","volume":"11","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-2991-0409","authenticated-orcid":false,"given":"Roger","family":"Davies","sequence":"first","affiliation":[{"name":"Department of Physics, University of Auckland, Auckland 1142, New Zealand"}]}],"member":"1968","published-online":{"date-parts":[[2018,12,26]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"1413","DOI":"10.1175\/1520-0469(1972)029<1413:CAAGCF>2.0.CO;2","article-title":"Cloudiness as a global feedback mechanism: The effects on the radiation balance and surface temperature of variations in cloudiness","volume":"29","author":"Schneider","year":"1972","journal-title":"J. Atmos. Sci."},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"L03701","DOI":"10.1029\/2011GL050506","article-title":"Global cloud height fluctuations measured by MISR on Terra from 2000 to 2010","volume":"39","author":"Davies","year":"2012","journal-title":"Geophys. Res. Lett."},{"key":"ref_3","doi-asserted-by":"crossref","first-page":"1031","DOI":"10.1175\/BAMS-D-12-00117.1","article-title":"Assessment of global cloud datasets from satellites: Project and database initiated by the GEWEX radiation panel","volume":"94","author":"Stubenrauch","year":"2013","journal-title":"Bull. Am. Meteorol. Soc."},{"key":"ref_4","doi-asserted-by":"crossref","first-page":"2189","DOI":"10.1175\/1520-0442(1999)012<2189:CASBSS>2.0.CO;2","article-title":"Clouds as seen by satellite sounders (3I) and imagers (ISCCP). Part I: Evaluation of cloud parameters","volume":"12","author":"Stubenrauch","year":"1999","journal-title":"J. Clim."},{"key":"ref_5","doi-asserted-by":"crossref","first-page":"2310","DOI":"10.1175\/2009JTECHA1281.1","article-title":"Overview of the CALIPSO mission and CALIOP data processing algorithms","volume":"26","author":"Winker","year":"2009","journal-title":"J. Atmos. Ocean. Technol."},{"key":"ref_6","doi-asserted-by":"crossref","first-page":"1532","DOI":"10.1109\/TGRS.2002.801150","article-title":"Operational retrieval of cloud-top heights using MISR data","volume":"40","author":"Moroney","year":"2002","journal-title":"IEEE Trans. Geosci. Remote Sens."},{"key":"ref_7","doi-asserted-by":"crossref","first-page":"3975","DOI":"10.1002\/2017JD026456","article-title":"Cloud heights measured by MISR from 2000 to 2015","volume":"122","author":"Davies","year":"2017","journal-title":"J. Geophys. Res."},{"key":"ref_8","doi-asserted-by":"crossref","first-page":"6133","DOI":"10.1175\/JCLI-D-14-00387.1","article-title":"Global seasonal precipitation anomalies robustly associated with El Ni\u00f1o and La Ni\u00f1a events\u2014An OLR perspective","volume":"28","author":"Chiodi","year":"2015","journal-title":"J. Clim."},{"key":"ref_9","unstructured":"(2018, December 25). Available online: http:\/\/www.bom.gov.au\/climate\/current\/soihtm1.shtml."},{"key":"ref_10","doi-asserted-by":"crossref","first-page":"553","DOI":"10.1002\/qj.828","article-title":"The ERA-Interim reanalysis: Configuration and performance of the data assimilation system","volume":"137","author":"Dee","year":"2011","journal-title":"Q. J. R. Meteorol. Soc."},{"key":"ref_11","doi-asserted-by":"crossref","first-page":"917","DOI":"10.1175\/1520-0442(1999)012<0917:RSSTVD>2.0.CO;2","article-title":"Remote Sea Surface Temperature Variations during ENSO: Evidence for a Tropical Atmospheric Bridge","volume":"12","author":"Klein","year":"1999","journal-title":"J. Clim."},{"key":"ref_12","doi-asserted-by":"crossref","first-page":"36","DOI":"10.1016\/j.dynatmoce.2006.06.003","article-title":"Tropical\u2013extratropical interactions related to upper-level troughs at low latitudes","volume":"43","author":"Knippertz","year":"2006","journal-title":"Dyn. Atmos. 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