{"id":11787,"date":"2024-05-10T10:04:24","date_gmt":"2024-05-10T01:04:24","guid":{"rendered":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/?p=11787"},"modified":"2024-06-20T12:14:30","modified_gmt":"2024-06-20T03:14:30","slug":"shang-ping-xie-2024-coupled-atmosphere-ocean-dynamics-from-el-nio-to-climate-change-%e6%9a%ab%e5%ae%9a%e3%83%a1%e3%83%a2","status":"publish","type":"post","link":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/?p=11787","title":{"rendered":"Shang-Ping Xie (2024) Coupled Atmosphere-Ocean Dynamics &#8212; From El Ni&ntilde;o to Climate Change (\u66ab\u5b9a\u30e1\u30e2)"},"content":{"rendered":"<ul>\n<li>Shang-Ping <strong>Xie<\/strong>, 2024: <em>Coupled Atmosphere-Ocean Dynamics: From El Ni&ntilde;o to Climate Change<\/em>. Elsevier, 424 pp. ISBN 978-0-323-95490-7 (paperback)<\/li>\n<\/ul>\n<p>\u6a2a\u306fB5\u306a\u307f\u3001\u7e26\u306fA5\u3088\u308a\u5c11\u3057\u5927\u304d\u3044\u5224\u306e\u30da\u30fc\u30d1\u30fc\u30d0\u30c3\u30af\u30022024\u5e74\u306e\u65b0\u520a\u3068\u306a\u3063\u3066\u3044\u308b\u304c2023\u5e74\u4e2d\u306b\u51fa\u3066\u3044\u305f\u3088\u3046\u3060\u3002\u308f\u305f\u3057\u306f2023\u5e7411\u6708\u306b\u901a\u4fe1\u8ca9\u58f2\u3067\u6ce8\u6587\u3057\u30012024\u5e741\u6708\u306b\u53d7\u3051\u53d6\u3063\u305f\u3002\u76ee\u6b21\u306e\u66f8\u304d\u629c\u304d\u3092\u3057\u305f\u304c\u3001\u307e\u3060\u5b9f\u8cea\u7684\u306b\u8aad\u3093\u3067\u3044\u306a\u3044\u3002\u3057\u304b\u3057\u3001\u56f3\u3092\u53c2\u7167\u3059\u308b\u3053\u3068\u304c\u3042\u308b\u306e\u3067\u3001\u66ab\u5b9a\u7248\u306e\u8aad\u66f8\u30e1\u30e2\u3092\u51fa\u3057\u3066\u304a\u304f\u3002<\/p>\n<p>\u8457\u8005\u306f\u4e2d\u56fd\u51fa\u8eab\u3067\u3001\u65e5\u672c\u3067\u535a\u58eb\u53f7\u3092\u3068\u3063\u305f\u3042\u3068\u3001\u30a2\u30e1\u30ea\u30ab\u5408\u8846\u56fd\u3067\u5927\u5b66\u6559\u54e1\u3092\u3057\u3066\u3044\u308b\u3002\u540d\u307e\u3048\u306f\u6f22\u5b57\u3067\u306f\u300c\u8b1d \u5c1a\u5e73\u300d\u3068\u304b\u304f\u3002\u300c\u8b1d (Xie)\u300d\u306e\u767a\u97f3\u3092 \u304b\u305f\u304b\u306a \u3067\u8fd1\u4f3c\u3059\u308c\u3070\u300c\u30b7\u30a8\u300d\u3067\u3042\u308b\u3002<\/p>\n<p>\u6298\u308a\u304b\u3048\u3057\u306e\u3042\u3068\u306b\u76ee\u6b21\u3092\u3064\u3051\u308b\u3002<br \/>\n<!--more--><br \/>\n===== \u76ee\u6b21 =====<br \/>\nContents<br \/>\nAcknowledgments<br \/>\nPreface<br \/>\n &#8211; &#8211; 1. Ocean-atmospehere coupling<br \/>\n &#8211; &#8211; 2. Aims of the book<br \/>\n &#8211; &#8211; 3. Organization<br \/>\n &#8211; &#8211; 4. Pedagogical features<br \/>\n1. Introduction<br \/>\n &#8211; 1.1 Role of the ocean in climate<br \/>\n &#8211; 1.2 Climate in the news<br \/>\n &#8211; 1.3 Fundamentals<br \/>\n &#8211; &#8211; 1.3.1 Geophysical fluid dynamics<br \/>\n &#8211; &#8211; 1.3.2 Ocean<br \/>\n &#8211; &#8211; 1.3.3 Atmosphere<br \/>\n &#8211; &#8211; &#8211; Isobaric coordinates<br \/>\n &#8211; &#8211; &#8211; Thermodynamic variables<br \/>\n &#8211; &#8211; 1.3.4 Air-sea exchange<br \/>\n &#8211; 1.4 General circulation models<br \/>\n &#8211; 1.5 Statistical methods<br \/>\n &#8211; &#8211; 1.5.1 Correlation<br \/>\n &#8211; &#8211; 1.5.2 Empirical orthogonal function<br \/>\n2. Energy balance and transport<br \/>\n &#8211; 2.1 Planetary energy balance and greenhouse effect<br \/>\n &#8211; 2.2 Radiative imbalance and energy transport<br \/>\n &#8211; 2.3 Ocean heat transport<br \/>\n &#8211; &#8211; 2.3.1 Ocean meridional overturning circulations<br \/>\n &#8211; &#8211; 2.3.2 Sea surface heat flux<br \/>\n &#8211; &#8211; [Box 2.1] Surface salinity<br \/>\n &#8211; 2.4 Atmospheric energy transport<br \/>\n &#8211; &#8211; 2.4.1 Tropics<br \/>\n &#8211; &#8211; [Box 2.2] Thermodynamic variables of the moist atmosphere<br \/>\n &#8211; &#8211; 2.4.2 Extratropics<br \/>\n &#8211; Review questions<br \/>\n3. Tropical convection and planetary-scale circulation<br \/>\n &#8211; 3.1 Water vapor budget<br \/>\n &#8211; 3.2 Ocean temperature effect on convection<br \/>\n &#8211; 3.3 Latent heat release in convection<br \/>\n &#8211; 3.4 Equatorial awves<br \/>\n &#8211; &#8211; 3.4.1 Two-level model<br \/>\n &#8211; &#8211; 3.4.2 Kelvin wave<br \/>\n &#8211; &#8211; 3.4.3 Rossby waves<br \/>\n &#8211; &#8211; 3.4.4 Wave dispersion<br \/>\n &#8211; &#8211; [Box 3.1] Discovery of equatorial waves<br \/>\n &#8211; 3.5 Planetary-scale circulation<br \/>\n &#8211; &#8211; 3.5.1 Response to an isolated heating<br \/>\n &#8211; &#8211; 3.5.2 Observed tropical circulation<br \/>\n &#8211; &#8211; 3.5.3 Rotational and divergent flow<br \/>\n &#8211; 3.6 Weak temperature gradient and convective threshold<br \/>\n &#8211; 3.7 Outlook<br \/>\n &#8211; Review questions<br \/>\n4. Madden-Julian oscillation<br \/>\n &#8211; 4.1 Convectively coupled waves<br \/>\n &#8211; &#8211; 4.1.1 Phase speed slowdown<br \/>\n &#8211; &#8211; 4.1.2 Kelvin wave<br \/>\n &#8211; &#8211; 4.1.3 Evaporation-wind feedback<br \/>\n &#8211; 4.2 Madden-Julian oscillation<br \/>\n &#8211; &#8211; 4.2.1 Circulation structure<br \/>\n &#8211; &#8211; 4.2.2 Zonal modulations<br \/>\n &#8211; &#8211; 4.2.3 Index<br \/>\n &#8211; &#8211; 4.2.4 Seasonality<br \/>\n &#8211; &#8211; 4.2.5 Ocean response<br \/>\n &#8211; &#8211; 4.2.6 Subseasonal prediction<br \/>\n &#8211; 5.3 Moisture mode theory<br \/>\n &#8211; Review questions<br \/>\n5. Summer Monsoons<br \/>\n &#8211; 5.1 South Asian monsoon<br \/>\n &#8211; &#8211; 5.1.1 Circulation<br \/>\n &#8211; &#8211; 5.1.2 Orographic effects on convection<br \/>\n &#8211; &#8211; 5.1.3 Onset<br \/>\n &#8211; &#8211; [Box 5.1] Land surface-atmosphere interactions<br \/>\n &#8211; 5.2 East Asian monsoon<br \/>\n &#8211; &#8211; 5.2.1 Thermal advection by the westerly jet<br \/>\n &#8211; &#8211; 5.2.2 Socioeconomic impacts<br \/>\n &#8211; &#8211; 5.2.3 Subtropical convection<br \/>\n &#8211; 5.3 Asian summer monsoon system<br \/>\n &#8211; &#8211; 5.3.1 Subsystems<br \/>\n &#8211; &#8211; 5.3.2 Connection to the Sahara Desert<br \/>\n &#8211; 5.4 West African monsoon<br \/>\n &#8211; 5.5 North American monsoon<br \/>\n &#8211; 5.6 Global monsoon<br \/>\n &#8211; 5.7 Discussion<br \/>\n &#8211; Review questions<br \/>\n6. Subtropical climate: Trade winds and low clouds<br \/>\n &#8211; 6.1 Trade wind climate<br \/>\n &#8211; 6.2 Cloud-regime transition<br \/>\n &#8211; 6.3 Climate feedback<br \/>\n &#8211; &#8211; 6.3.1 Cloud-SST feedback<br \/>\n &#8211; &#8211; 6.3.2 Global radiative feedback<br \/>\n &#8211; 6.4 California climate<br \/>\n &#8211; &#8211; 6.4.1 Coastal upwelling<br \/>\n &#8211; &#8211; 6.4.2 Atmospheric rivers<br \/>\n &#8211; &#8211; 6.4.2 Hydroclimate<br \/>\n &#8211; Review questions<br \/>\n7. Equatorial oceanography<br \/>\n &#8211; 7.1 Dynamical models<br \/>\n &#8211; &#8211; 7.1.1 Equatorial upwelling<br \/>\n &#8211; &#8211; 7.1.2 Thermal stratification<br \/>\n &#8211; &#8211; 7.1.3 Phressure perturbation due to thermocline displacements<br \/>\n &#8211; &#8211; 7.1.4 1.5-layer reduced-gravity model<br \/>\n &#8211; &#8211; 7.1.5 2.5-layer model<br \/>\n &#8211; 7.2 Ocean response to wind stress forcing<br \/>\n &#8211; &#8211; 7.2.1 Currents at the equator<br \/>\n &#8211; &#8211; 7.2.2 Yoshida jet<br \/>\n &#8211; &#8211; 7.2.3 Wave adjustments with meridional boundaries<br \/>\n &#8211; &#8211; 7.2.4 Ocean adjustments with meridional boundaries<br \/>\n &#8211; &#8211; 7.2.5 Long Rossby waves and Sverdrup balance<br \/>\n &#8211; &#8211; 7.2.6 Equatorial current system<br \/>\n &#8211; 7.3 Mixed-layer heat budget<br \/>\n &#8211; &#8211; 7.3.1 Governeing equation<br \/>\n &#8211; &#8211; 7.3.2 Surface heat flux<br \/>\n &#8211; Review questions<br \/>\n8. Coupled feedbacks and tropical climatology<br \/>\n &#8211; 8.1 Meridional asymmetry<br \/>\n &#8211; &#8211; 8.1.1 Wind-evaporation-{sea surface temperature} feedback<br \/>\n &#8211; &#8211; 8.1.2 Coupled model<br \/>\n &#8211; &#8211; 8.1.3 Continental forcing and the westward control<br \/>\n &#8211; &#8211; 8.1.4 Tropical basin view vs. global zonal-mean theory<br \/>\n &#8211; 8.2 Equatorial cold tongue and Walker circulation<br \/>\n &#8211; 8.3 Equatorial annual cycle<br \/>\n &#8211; &#8211; [Box 8.1] Climate on the Galapagos<br \/>\n &#8211; &#8211; 8.3.1 Annual frequency<br \/>\n &#8211; &#8211; 8.3.2 Westward phase propagation<br \/>\n &#8211; &#8211; 8.3.3 Broad seasonal variations<br \/>\n &#8211; Review questions<br \/>\n9. El Ni&ntilde;o, the Southern Oscillation, and the global influence<br \/>\n &#8211; [Box 9.1] Road to coupled dynamics<br \/>\n &#8211; 9.1 1997-1998 El Ni&ntilde;o<br \/>\n &#8211; 9.2 Bjerknes feedback<br \/>\n &#8211; &#8211; 9.2.1 Effect of Earth rotation<br \/>\n &#8211; &#8211; 9.2.2 Ocean heat budget and coupled instability<br \/>\n &#8211; 9.3 Mechanisms for oscillation<br \/>\n &#8211; 9.4 Life cycle<br \/>\n &#8211; &#8211; 9.4.1 Seasonal phase locking<br \/>\n &#8211; &#8211; 9.4.2 Trigering mechanisms<br \/>\n &#8211; &#8211; 9.4.3 ENSO diversity<br \/>\n &#8211; &#8211; 9.4.4 Spring convective view<br \/>\n &#8211; 9.5 global influences<br \/>\n &#8211; &#8211; 9.5.1 Tropics<br \/>\n &#8211; &#8211; 9.5.2 Pacific North American pattern<br \/>\n &#8211; &#8211; 9.5.3 Ocean waveguide<br \/>\n &#8211; 9.6 Barotropic stationary waves in the westerlies<br \/>\n &#8211; &#8211; 9.6.1 Energy dispersion<br \/>\n &#8211; &#8211; 9.6.2 Rossby wave source<br \/>\n &#8211; &#8211; 9.6.3 Geographic anchor<br \/>\n &#8211; &#8211; 9.6.4 Seasonality<br \/>\n &#8211; 9.7 Seasonal prediction<br \/>\n &#8211; 9.8 Summary remarks<br \/>\n &#8211; Review questions<br \/>\n10. Tropical Atlantic variability<br \/>\n &#8211; 10.1 Seasonal cycle<br \/>\n &#8211; &#8211; 10.1.1 Intertropical convergence zone<br \/>\n &#8211; &#8211; 10.1.2 Equatorial cold tongue<br \/>\n &#8211; &#8211; 10.1.3 Easterly winds over the equatorial Gulf of Guinea<br \/>\n &#8211; 10.2 Zonal mode: Atlantic Ni&ntilde;o<br \/>\n &#8211; 10.3 Meridional mode<br \/>\n &#8211; 10.4 Interactions with the Pacific<br \/>\n &#8211; &#8211; 10.4.1 ENSO influence<br \/>\n &#8211; &#8211; 10.4.2 Influence on the Pacific<br \/>\n &#8211; 10.5 Climate modulation of tropical cyclones<br \/>\n &#8211; &#8211; [Box 10.1] Coupled modes in forecast ensemble spread<br \/>\n &#8211; &#8211; 10.5.1 Genesis potential<br \/>\n &#8211; &#8211; 10.5.2 Dynamics of wind shear<br \/>\n &#8211; &#8211; 10.5.3 Interannual variability<br \/>\n &#8211; &#8211; 10.5.4 Ocean feedback<br \/>\n &#8211; 10.6 Summary<br \/>\n &#8211; Review questions<br \/>\n11. Indian Ocan variability<br \/>\n &#8211; 11.1 Seasonal cycle<br \/>\n &#8211; 11.2 Zonal mode: Indian Ocean dipole<br \/>\n &#8211; 11.3 Basin mode<br \/>\n &#8211; &#8211; 11.3.1 Thermocline ridge<br \/>\n &#8211; &#8211; 11.3.2 Wind-evaporation-{sea surface temperature} (WES) feedback in boreal spring<br \/>\n &#8211; 11.4 Post-ENSO summer capacitor effect<br \/>\n &#8211; &#8211; 11.4.1 Indian Ocean effect on the atmosphere<br \/>\n &#8211; &#8211; 11.4.2 Regional ocean-atmosphere coupling<br \/>\n &#8211; &#8211; [Box 11.1] An instrinsic mode to the summer monsoon<br \/>\n &#8211; &#8211; 11.4 3 Prediction<br \/>\n &#8211; 11.5 Asian summer monsoon variability<br \/>\n &#8211; &#8211; 11.5.1 India<br \/>\n &#8211; &#8211; 11.5.2 China<br \/>\n &#8211; 11.6 Synthesis<br \/>\n &#8211; Review questions<br \/>\n12. Extratropical variability and the influence on the tropics<br \/>\n &#8211; 12.1 Atmospheric internal variability<br \/>\n &#8211; 12.2 Atmospheric forcing of SST: Lagged correlation diagnosis<br \/>\n &#8211; &#8211; 12.2.1 Stochastic model 1 without positive feedback<br \/>\n &#8211; &#8211; 12.2.2 Lagged corralation<br \/>\n &#8211; &#8211; 12.2.3 Stochastic model 2 with ocean feedback<br \/>\n &#8211; &#8211; 12.2.4 Observed cross-correlation<br \/>\n &#8211; &#8211; [Box 12.1] Evolving views on extratropical variability<br \/>\n &#8211; 12.3 Ocean dynamic effects<br \/>\n &#8211; &#8211; 12.3.1 Ocean Rossby waves<br \/>\n &#8211; &#8211; [Box 12.2] Ocean front-atmosphere interaction<br \/>\n &#8211; &#8211; 12.3.2 Atlantic Multidecadal Oscillation<br \/>\n &#8211; 12.4 Extratropical influence on tropical climate<br \/>\n &#8211; &#8211; 12.4.1 Pacific meridional mode<br \/>\n &#8211; &#8211; 12.4.2 Cross-equatorial energy transport<br \/>\n &#8211; 12.5 Deep meridional overturning circulation<br \/>\n &#8211; 12.6 Summary remarks<br \/>\n &#8211; Review questions<br \/>\n13. Gloabl Warming: Thermodynamic Effects<br \/>\n &#8211; 13.1 Climate feedback analysis<br \/>\n &#8211; &#8211; [Box 13.1] Coupled Model Intercomparison Project and radiative forcing scenarios<br \/>\n &#8211; &#8211; 13.1.1 Equilibrium response<br \/>\n &#8211; &#8211; 13.1.2 Transient response<br \/>\n &#8211; &#8211; 13.1.3 Abrupt CO<sub>2<\/sub> increase experiment<br \/>\n &#8211; 13.2 Global warming hiatus<br \/>\n &#8211; &#8211; 13.2.1 Tropical Pacific pacemaker effect<br \/>\n &#8211; &#8211; 13.2.2 Planetary energetics<br \/>\n &#8211; &#8211; 13.2.3 Estimating anthropogenic warming<br \/>\n &#8211; 13.3. RObust atmospheric changes due to thermodynamic effects<br \/>\n &#8211; &#8211; 13.3.1 Enhanced warming over land<br \/>\n &#8211; &#8211; 13.3.2 Heatwaves<br \/>\n &#8211; &#8211; 13.3.3 Arctic amplification<br \/>\n &#8211; &#8211; 13.3.4 Hydrologic cycle<br \/>\n &#8211; &#8211; 13.3.5 Slowdown of Walker circulation<br \/>\n &#8211; &#8211; 13.3.6 Extreme precipitation<br \/>\n &#8211; &#8211; 13.3.7 Vertical structure of the tropospheric warming<br \/>\n &#8211; &#8211; 13.3.8 Expansion of subtropical dry zones<br \/>\n &#8211; 13.4 Surface acceleration of the subtropical ocean gyre<br \/>\n &#8211; 13.5 Discussion<br \/>\n &#8211; Review questions<br \/>\n14. Regional climate change<br \/>\n &#8211; 14.1 Regional patterns of tropical rainfall change<br \/>\n &#8211; 14.2 SST pattern dynamics<br \/>\n &#8211; &#8211; 14.2.1 El Ni&ntilde;o and Southern Oscillation (ENSO) changes<br \/>\n &#8211; &#8211; 14.2.2 El Ni&ntilde;o-like warming<br \/>\n &#8211; &#8211; 14.2.3 Indian Ocean Dipole (IOD) -like warming<br \/>\n &#8211; 14.3 Regional uncertainty due to anthropogenic circulation change<br \/>\n &#8211; &#8211; 14.3.1 SST pattern<br \/>\n &#8211; &#8211; 14.3.2 Internal variability<br \/>\n &#8211; 14.4 Ocean heat uptake<br \/>\n &#8211; &#8211; 14.4.1 Response to greenhouse forcing<br \/>\n &#8211; &#8211; 14.4.2 Cross-equatorial energy transport<br \/>\n &#8211; 14.5 Aerosol effects<br \/>\n &#8211; &#8211; 14.5.1 Interhemispheric asymmetry<br \/>\n &#8211; &#8211; 14.5.2 Ocean dynamic feedback<br \/>\n &#8211; &#8211; 14.5.3 Evolving distribution<br \/>\n &#8211; 14.6 Historical climate change<br \/>\n &#8211; 14.7 Synthesis<br \/>\n &#8211; Review questions<br \/>\nEpilogue<br \/>\n &#8211; &#8211; Sponeaneous oscillations<br \/>\n &#8211; &#8211; Energy view<br \/>\n &#8211; &#8211; Outlook<br \/>\n &#8211; &#8211; Now I see<br \/>\nReferences<br \/>\nIndex<br \/>\n==========<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Shang-Ping Xie, 2024: Coupled Atmosphere-Ocean Dynamics: From El Ni&ntilde;o to Climate Change. Elsevier, 424  [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-11787","post","type-post","status-publish","format-standard","hentry","category-dokusyo-memo-"],"_links":{"self":[{"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=\/wp\/v2\/posts\/11787","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=11787"}],"version-history":[{"count":7,"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=\/wp\/v2\/posts\/11787\/revisions"}],"predecessor-version":[{"id":11894,"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=\/wp\/v2\/posts\/11787\/revisions\/11894"}],"wp:attachment":[{"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=11787"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=11787"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/macroscope.world.coocan.jp\/yukukawa\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=11787"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}