Jing Chen, Robert H. Weisberg, Lianyuan Zheng, Chuanmin Hu, Yingjun Zhang, Alexander K. Nickerson, Jeffrey C. Donovan, Yonggang Liu
Surface fronts are common features across the world's oceans, particularly in estuarine and coastal regions where the merging of freshwater and saltwater creates strong density gradients. It has long been documented that fronts in these regions can trap and concentrate various properties such as floating debris, nutrients, larvae, and other buoyant materials. The prediction of such fronts has important implications for environmental protection, search and rescue operations, and scientific research. However, the realistic simulation of such features remains a challenge. In this study, we apply a high-resolution, numerical circulation model of Tampa Bay and the adjacent West Florida Shelf to predict surface fronts by computing surface convergence. The accuracy of the simulation is evaluated using drone and satellite imagery. The simulated convergence fields are then analyzed by a Self-Organizing Map, an unsupervised machine learning method. Our findings show that convergence patterns vary with tidal phases (ebb and flood) as well as the spring–neap tidal cycle. This study provides a new framework for improving monitoring strategies and reducing observational bias. Although every estuary is unique, the physical mechanisms of frontogenesis are universal. Therefore, the method we propose can be applied to other estuarine systems and serve as a valuable tool for interdisciplinary research in estuarine and coastal environments.
{"title":"Frontogenesis by material convergence in an estuary and its adjacent coastal ocean","authors":"Jing Chen, Robert H. Weisberg, Lianyuan Zheng, Chuanmin Hu, Yingjun Zhang, Alexander K. Nickerson, Jeffrey C. Donovan, Yonggang Liu","doi":"10.1002/lno.70276","DOIUrl":"10.1002/lno.70276","url":null,"abstract":"<p>Surface fronts are common features across the world's oceans, particularly in estuarine and coastal regions where the merging of freshwater and saltwater creates strong density gradients. It has long been documented that fronts in these regions can trap and concentrate various properties such as floating debris, nutrients, larvae, and other buoyant materials. The prediction of such fronts has important implications for environmental protection, search and rescue operations, and scientific research. However, the realistic simulation of such features remains a challenge. In this study, we apply a high-resolution, numerical circulation model of Tampa Bay and the adjacent West Florida Shelf to predict surface fronts by computing surface convergence. The accuracy of the simulation is evaluated using drone and satellite imagery. The simulated convergence fields are then analyzed by a Self-Organizing Map, an unsupervised machine learning method. Our findings show that convergence patterns vary with tidal phases (ebb and flood) as well as the spring–neap tidal cycle. This study provides a new framework for improving monitoring strategies and reducing observational bias. Although every estuary is unique, the physical mechanisms of frontogenesis are universal. Therefore, the method we propose can be applied to other estuarine systems and serve as a valuable tool for interdisciplinary research in estuarine and coastal environments.</p>","PeriodicalId":18143,"journal":{"name":"Limnology and Oceanography","volume":"71 1","pages":""},"PeriodicalIF":3.7,"publicationDate":"2025-11-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://aslopubs.onlinelibrary.wiley.com/doi/epdf/10.1002/lno.70276","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145598707","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Meredith A. Holgerson, Nicholas E. Ray, Kathryn A. Gannon, Adam J. Heathcote
Ponds influence global carbon (C) cycling due to high rates of organic C (OC) burial and carbon dioxide (CO2) and methane (CH4) emissions. Here, we quantified OC burial rates and CO2 and CH4 concentrations and fluxes in two ponds that were similar in size and gross primary production, but differed in depth and dominant primary producers. The deeper (3.9 m) Texas Hollow Pond was phytoplankton dominated with stronger and longer (143 d) stratification compared to the shallower (2.7 m) macrophyte-dominated Mud Pond (85 d). Both ponds exhibited high CO2 and CH4 emissions and high OC burial, yet C pathways differed. Strong stratification in Texas Hollow Pond led to anoxic bottom waters, benthic CO2 and CH4 accumulation, and limited OC decomposition, whereas Mud Pond remained oxygenated with similar gas concentrations across the water column. Texas Hollow Pond had 2.6 times higher CO2 emissions than Mud Pond, perhaps related to greater wetland C inputs in Texas Hollow. Despite similar diffusive CH4 emissions between ponds, the weakly stratified Mud Pond had twice as much CH4 ebullition, likely due to warmer waters and macrophyte-derived OC fueling methanogenesis. In summary, slight differences in depth and light attenuation can regulate stratification, plant communities, oxygen availability, and C processing in ponds. Given that ponds are hotspots for C cycling and are sensitive to climate-driven changes in stratification, understanding the mechanisms behind C processing is critical for local management and predicting global C budgets.
{"title":"Carbon fluxes in two temperate ponds are mediated by stratification and primary producers","authors":"Meredith A. Holgerson, Nicholas E. Ray, Kathryn A. Gannon, Adam J. Heathcote","doi":"10.1002/lno.70273","DOIUrl":"10.1002/lno.70273","url":null,"abstract":"<p>Ponds influence global carbon (C) cycling due to high rates of organic C (OC) burial and carbon dioxide (CO<sub>2</sub>) and methane (CH<sub>4</sub>) emissions. Here, we quantified OC burial rates and CO<sub>2</sub> and CH<sub>4</sub> concentrations and fluxes in two ponds that were similar in size and gross primary production, but differed in depth and dominant primary producers. The deeper (3.9 m) Texas Hollow Pond was phytoplankton dominated with stronger and longer (143 d) stratification compared to the shallower (2.7 m) macrophyte-dominated Mud Pond (85 d). Both ponds exhibited high CO<sub>2</sub> and CH<sub>4</sub> emissions and high OC burial, yet C pathways differed. Strong stratification in Texas Hollow Pond led to anoxic bottom waters, benthic CO<sub>2</sub> and CH<sub>4</sub> accumulation, and limited OC decomposition, whereas Mud Pond remained oxygenated with similar gas concentrations across the water column. Texas Hollow Pond had 2.6 times higher CO<sub>2</sub> emissions than Mud Pond, perhaps related to greater wetland C inputs in Texas Hollow. Despite similar diffusive CH<sub>4</sub> emissions between ponds, the weakly stratified Mud Pond had twice as much CH<sub>4</sub> ebullition, likely due to warmer waters and macrophyte-derived OC fueling methanogenesis. In summary, slight differences in depth and light attenuation can regulate stratification, plant communities, oxygen availability, and C processing in ponds. Given that ponds are hotspots for C cycling and are sensitive to climate-driven changes in stratification, understanding the mechanisms behind C processing is critical for local management and predicting global C budgets.</p>","PeriodicalId":18143,"journal":{"name":"Limnology and Oceanography","volume":"71 1","pages":""},"PeriodicalIF":3.7,"publicationDate":"2025-11-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145598706","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}