Severity: Warning
Message: file_get_contents(https://...@gmail.com&api_key=61f08fa0b96a73de8c900d749fcb997acc09&a=1): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests
Filename: helpers/my_audit_helper.php
Line Number: 197
Backtrace:
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 197
Function: file_get_contents
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 271
Function: simplexml_load_file_from_url
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 1075
Function: getPubMedXML
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 3195
Function: GetPubMedArticleOutput_2016
File: /var/www/html/application/controllers/Detail.php
Line: 597
Function: pubMedSearch_Global
File: /var/www/html/application/controllers/Detail.php
Line: 511
Function: pubMedGetRelatedKeyword
File: /var/www/html/index.php
Line: 317
Function: require_once
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Current carbon flux data for China's terrestrial ecosystems have limitations, such as short time series and low resolution. Generating longer time series and higher-resolution carbon flux data for these ecosystems is crucial for studying their temporal and spatial variation characteristics and for analyzing the impact of land use changes on carbon fluxes. This study constructed four machine learning models using flux data from Chinese sites and relevant predictor variables, identifying the random forest model as the best predictive model. The values for the training and test sets were 0.73 and 0.77, respectively, with RMSE (in C) values of 35.09 g·(m·month) and 32.85 g·(m·month). The model was validated through ten-fold cross-validation and leave-one-site-out cross-validation, and it was subsequently used to generate a monthly carbon flux prediction dataset for China's terrestrial ecosystems at 1 km resolution from 2000 to 2020. The results showed a decreasing trend in terrestrial carbon sinks from southeast to northwest China between 2000 and 2020, with the largest carbon sinks located in southern monsoon regions, North China, and the northeastern mountains. Inner Mongolia and the interior Tibetan Plateau are weak carbon sources, whereas Xinjiang and the northeastern Tibetan Plateau are stronger carbon sources. Terrestrial carbon sinks are influenced by climate factors, showing distinct seasonal variations. Over the past 20 years, China's terrestrial carbon sinks (in C) ranged from 0.38 to 0.77 Pg·a, with an overall increasing trend. Analysis of land use data revealed that forests have the strongest carbon sinks, followed by croplands and built-up areas. Grasslands are weak carbon sources, and unused lands are strong carbon sources. Changes in land use types significantly impact terrestrial carbon sinks. Rational land use policies help increase carbon sinks, contributing to climate change mitigation and ecological environment protection.
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http://dx.doi.org/10.13227/j.hjkx.202406133 | DOI Listing |