{"id":450,"date":"2022-08-12T17:50:16","date_gmt":"2022-08-12T09:50:16","guid":{"rendered":"https:\/\/byjoydesign.com\/chia\/?page_id=450"},"modified":"2022-08-12T20:09:12","modified_gmt":"2022-08-12T12:09:12","slug":"2022-poster","status":"publish","type":"page","link":"https:\/\/hydro.as.ntu.edu.tw\/chia\/forum-2022\/2022-poster\/","title":{"rendered":"CHiA Forum 2022 Poster"},"content":{"rendered":"\t\t
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Day 2<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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8\/18
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\u6642\u9593\uff1a2022\/08\/17-2022\/08\/19<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t

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Poster Section<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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poster I (\u55ae\u865f)\u3001poster II (\u96d9\u865f)<\/div>\n\n\t\t\t\t\t\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
1<\/td>Yu-Hung Chang<\/td>Deep-inflow Mixing Features of Orographic Locking Diurnal Convection<\/td><\/tr>
2<\/td>Shao-Yu Tseng<\/td>The Multi-scale Interactions between the Long-lived Convective Systems and the Northwest Pacific Monsoon Trough: Satellite Observation Perspectives<\/td><\/tr>
3<\/td>\u8a31 \u6840 (Jie Hsu)<\/td>The progress of satellite precipitation products in monitoring multi-timescale precipitation variations over Taiwan<\/td><\/tr>
4<\/td>chen peng jen<\/td>Machine Learning Detection of Fog\/Low cloud over E Taiwan Mountains from Himawari-8 Satellite True-color Images<\/td><\/tr>
5<\/td>Chi-Huan Hsu<\/td>Evaluating the Convectively Coupled Equatorial Rossby Waves in the Hindcasts of Global Models with Different Convection Representations from a Lagrangian Perspective<\/td><\/tr>
6<\/td>\u5f35\u4fca\u6770<\/td>The mechanism study of wintertime heavy pricipitation in Yilan by idealized large eddy simulations<\/td><\/tr>
7<\/td>\u59dc\u79ae\u5f37<\/td>MJO\u7684\u6c23\u5019\u8b8a\u7570<\/td><\/tr>
8<\/td>Cheng Wei Lin<\/td>Estimation of wind and solar energy in Taiwan: Extremely high-resolution climate change projection<\/td><\/tr>
9<\/td>Hung Peng Tsai<\/td>Projections of historical typhoon change under pseudo global warming +2\u00b0C & +4\u00b0C scenario<\/td><\/tr>
10<\/td>\u9673\u4fde\u7db8<\/td>only position<\/td><\/tr>
11<\/td>Sieu-Cuong San<\/td>Extratropical-tropical interaction via the propagation of subsurface spiciness anomalies in the North Pacific<\/td><\/tr>
12<\/td>\u674e\u6b63\u5b89<\/td>Impact of multiple-scale circulation interactions on the spring diurnal precipitation over Luzon<\/td><\/tr>
13<\/td>\u90ed\u4f73\u6b23<\/td>An Indirect Path to Precipitation Reconstruction under SSWF using Large-Scale Environments<\/td><\/tr>
14<\/td>Yu-Hsiu Wang<\/td>Deep-inflow Features of Afternoon Thunderstorm in Mountain Area under Ideal Terrain Model.<\/td><\/tr>
15<\/td>\u6797\u6dd1\u8ed2(Shu-Hsuan,Lin)<\/td>(Poster)MSE Budget Analysis of Strong and Weak MJO Events Using ERA5 and COSMIC RO Data: A Case-to-Case Comparison Study<\/td><\/tr>
16<\/td>He-Ming Xiao<\/td>Remote response of Maritime Continent\u2019s deforestation to the Northern Pacific in December<\/td><\/tr>
17<\/td>Chun-Shiung Weng<\/td>Intraseasonal Atmospheric Forcing on Upper Ocean Circulation and Heat Content over the Tropical Northwestern Pacific Ocean<\/td><\/tr>
18<\/td>\u5f90\u5b50\u6db5<\/td>The Observation Based Index to Investigate the Role of the Lee Vortex in Enhancing Air Pollution over Northwestern Taiwan<\/td><\/tr>
19<\/td>\u6c5f\u921e<\/td>CMIP6\u5c0d\u6771\u4e9e\u590f\u5b63\u5b63\u98a8\u7684\u591a\u91cd\u6642\u9593\u5c3a\u5ea6\u6a21\u64ec\u80fd\u529b\u4e4b\u8a55\u4f30\u8207\u672a\u4f86\u8b8a\u9077 (poster)<\/td><\/tr>
20<\/td>\u8523\u6fec\u6fc2<\/td>The Role of Climate Mean-State on the Anthropogenic Land-use Change Induced Hydroclimate Changes in the Maritime Continent<\/td><\/tr>
21<\/td>Jo Hsu Huang \u9ec3\u504c\u6829<\/td>Change and variability of Kuroshio under global warming<\/td><\/tr>
22<\/td>Dian-You Chen<\/td>The seasonal dependency of tropical transient response to an idealized extratropical thermal forcing in fully coupled CESM<\/td><\/tr>
23<\/td>\u9673\u82f1\u5a77<\/td>\u53f0\u7063\u6c23\u6eab\u5b63\u7bc0\u5faa\u74b0\u7684\u9577\u671f\u8b8a\u9077<\/td><\/tr>
24<\/td>Hung-Yi Tseng<\/td>Fast and Slow Responses of the Tropical Pacific to Radiative Forcing in High Latitudes<\/td><\/tr>
25<\/td>\u8b1d\u627f\u52f3<\/td>\u5f85\u5b9a<\/td><\/tr>
26<\/td>An-Yi Huang<\/td>Can PMM Always be a Precursor and Predictor of ENSO? (Poster)<\/td><\/tr>
27<\/td>\u9673\u6c38\u771f<\/td>Seasonal Dependency of Hadley Circulation Responses to High Latitude Forcing<\/td><\/tr>
28<\/td>\u674e\u6df3\u5f18\uff08Chun-Hung Li)<\/td>Exploring nonlinearities in the climate responses under different magnitudes of deforestation in Maritime Continent<\/td><\/tr>
29<\/td>Jang, Yi-Shin<\/td>The effect of forest in dampening the diurnal cycle on land-atmosphere interaction<\/td><\/tr>
30<\/td>\u9673\u67cf\u5112<\/td>Understanding the Temporal Evolution of Tropical Pacific Responses to Anthropogenic Sulfate Aerosol Emission<\/td><\/tr>
31<\/td>Chia-Wei Lan<\/td>The Reduced Seasonality Over the Pan-arctic Region Under Global Warming<\/td><\/tr>
32<\/td>Ren-Jie Wu<\/td>South Asia suffers severe water scarcity even under the Paris Agreement<\/td><\/tr>
33<\/td>\u738b\u9038<\/td>Exploring the Differences of between Stratospheric Sudden Warmings in High-top and Low-top Climate Models<\/td><\/tr>
34<\/td>\u5468\u5b50\u6db5<\/td>to be determined<\/td><\/tr>
35<\/td>\u65bd\u749f\u5b8f<\/td>The Unique Diurnal Relative Humidity Characteristics in Coastal Montane Region<\/td><\/tr>
36<\/td>Mohammed Abdul Athick AS<\/td>Trend of Ocean Current and Sea Surface Temperature of Kuroshio Extent Delineated Using a Combination of Spatial Domain Filters.<\/td><\/tr><\/tbody><\/table><\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t13:30 poster I (\u55ae\u865f) \u300115:30 poster II (\u96d9\u865f)\t\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/h4>\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Day 2 8\/18 Thursday \u5730\u9ede\uff1a\u4e2d\u7814\u9662\u4eba\u6587\u9928\u5357\u68df3\u6a13\u7b2c\u4e8c\u6703\u8b70\u5ba4 \u6642\u9593\uff1a2022\/08\/17-20 […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":441,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"ocean_post_layout":"full-screen","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"on","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"default","ocean_display_header":"default","ocean_header_style":"","ocean_center_header_left_menu":"0","ocean_custom_header_template":"0","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":400,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0","osh_disable_topbar_sticky":"default","osh_disable_header_sticky":"default","osh_sticky_header_style":"default","osh_sticky_header_effect":"","osh_custom_sticky_logo":0,"osh_custom_retina_sticky_logo":0,"osh_custom_sticky_logo_height":0,"osh_background_color":"","osh_links_color":"","osh_links_hover_color":"","osh_links_active_color":"","osh_links_bg_color":"","osh_links_hover_bg_color":"","osh_links_active_bg_color":"","osh_menu_social_links_color":"","osh_menu_social_hover_links_color":"","slim_seo":{"title":"CHiA Forum 2022 Poster - Climate Hotpots in Action (CHiA) Forum","description":"Day 2 8\/18 Thursday \u5730\u9ede\uff1a\u4e2d\u7814\u9662\u4eba\u6587\u9928\u5357\u68df3\u6a13\u7b2c\u4e8c\u6703\u8b70\u5ba4 \u6642\u9593\uff1a2022\/08\/17-2022\/08\/19 8\/17 WEN 8\/18 THU 8\/19 FRI Poster Section poster I (\u55ae\u865f)\u3001poster II (\u96d9\u865f) 1 Yu-Hung Chang Deep-infl"},"footnotes":""},"class_list":["post-450","page","type-page","status-publish","hentry","entry"],"_links":{"self":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages\/450","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/comments?post=450"}],"version-history":[{"count":0,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages\/450\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages\/441"}],"wp:attachment":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/media?parent=450"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}