{"id":347,"date":"2018-03-28T20:26:09","date_gmt":"2018-03-29T00:26:09","guid":{"rendered":"http:\/\/hydrouncertainty.org\/?p=347"},"modified":"2019-01-15T10:44:59","modified_gmt":"2019-01-15T15:44:59","slug":"grand-challenges","status":"publish","type":"post","link":"http:\/\/hydrouncertainty.org\/2018\/03\/28\/grand-challenges\/","title":{"rendered":"Grand challenges"},"content":{"rendered":"\n
Substantial progress has been made in the last several decades for quantification and communication of hydrologic uncertainty (uncertainty quantification here is in a broad sense, including parameter estimation, sensitivity analysis, uncertainty propagation, and experimental data and data-worth analysis for uncertainty reduction). For example, due to development of public-domain software (e.g., PEST, UCODE, and DREAM), uncertainty quantification using regression and Bayesian methods has become a common practice not only in academic but also in consulting industry and govern agencies. However, the hydrologic uncertainty community are still facing several grand challenges that have not been fully resolved, and new challenges emerge due to changing hydrology and environmental conditions. Below are three grand challenges that may be addressed in the coming decade:<\/p>\n\n\n\n
Substantial progress has been made in the last several decades for quantification and communication of hydrologic uncertainty (uncertainty quantification here is in a broad sense, including parameter estimation, sensitivity analysis, uncertainty propagation, and experimental data and data-worth analysis for uncertainty<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0},"categories":[8],"tags":[],"jetpack_featured_media_url":"","_links":{"self":[{"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/posts\/347"}],"collection":[{"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/comments?post=347"}],"version-history":[{"count":2,"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/posts\/347\/revisions"}],"predecessor-version":[{"id":349,"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/posts\/347\/revisions\/349"}],"wp:attachment":[{"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/media?parent=347"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/categories?post=347"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/hydrouncertainty.org\/wp-json\/wp\/v2\/tags?post=347"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}