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E-commerce","智能客服：通过自然语言对话理解用户需求，提供产品推荐、订单查询、退换货支持等服务，提升客户满意度。\n个性化营销推荐：基于用户浏览、购买、偏好等行为数据，生成个性化推荐内容与优惠策略，提高转化率和客单价。\n商品内容生成：自动撰写商品标题、卖点描述、使用说明等内容，适用于海量SKU的内容生产与多语言发布。","buy",{"id":520,"value":520,"name":521,"intro":522,"add_value":523,"describe":8},10,"Security & Protection",null,"safe-shield-line",{"id":525,"value":525,"name":526,"intro":522,"add_value":527,"describe":8},11,"Environment & Climate","weather",{"id":529,"value":529,"name":530,"intro":522,"add_value":531,"describe":8},12,"Energy & Resource","energy-leaf",{"id":533,"value":533,"name":534,"intro":522,"add_value":535,"describe":8},13,"Express & Logistics","speed-outline",{"id":537,"value":537,"name":538,"intro":522,"add_value":539,"describe":8},15,"Sports","baseball-outline",{"id":541,"value":541,"name":542,"intro":522,"add_value":543,"describe":8},16,"General Data","daily-booth",{"id":545,"value":545,"name":546,"intro":522,"add_value":547,"describe":8},17,"Content & 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Culture","lang",{"id":564,"unique_code":565,"title":566,"icon":8,"intro":567,"cate":483,"detail":568,"create_time":569,"update_time":570,"price":571,"view_count":572,"download_count":573,"unit":573,"amount":574,"is_create_order":573,"enterprise_id":488,"seo_keywords":575,"seo_description":576,"data_format":577,"file_size":578,"apply_scene":579,"training_task":580,"version":581,"dataset_type_id":492,"dataset_scene_id":525,"sample_file":522,"banner":8,"unit_name":8,"cate_name":449,"icon_url":8,"banner_url":8,"sample_file_url":8,"data_dict":582,"qa_list":618,"sample_metadatas":635,"text_sample_content":668,"enterprise_name":669,"enterprise_logo":670,"data_distribution":671},1059,"abdde09816b7d28222858b9b48302cc9","Satellite Observation Q&A Dataset for Convective Initiation Diagnosis","Diagnose possible triggers of new convection from satellite time-series clues, with evidence and uncertainty clearly identified.","\u003Cp>This dataset turns meteorological satellite time-series clues, such as cloud development, cooling cloud tops, and localized cloud expansion, into diagnostic question-and-answer examples focused on possible triggers of new convection. Each record covers the observed clues, a diagnostic question, a possible mechanism, conclusions supported by the observations, unresolved factors, and the reasoning process, while distinguishing observations from inferences. It supports abductive reasoning research in satellite meteorology, reasoning SFT, model evaluation, and diagnostic Q&A system development.\u003C\u002Fp>","2026-10-09 17:19:12","2026-10-19 18:26:49","0.00",34,0,5000,"satellite observation dataset, convective initiation diagnosis, meteorological satellite data, convection triggering, abductive reasoning, cloud-top cooling, reasoning SFT, meteorological Q&A","Satellite observation Q&A for convective initiation diagnosis, covering time-series clues, possible mechanisms, supporting evidence, and uncertainty for meteor,","JSON","0.3GB","satellite weather monitoring, convective initiation diagnosis, severe weather analysis","visual question answering, meteorological reasoning, uncertainty assessment","V1.0",[583,588,593,598,603,608,613],{"id":573,"name":584,"field":585,"intro":586,"type":587},"File Name","file_name","File name","string",{"id":589,"name":590,"field":591,"intro":592,"type":587},7700,"Unresolved Factors","uncertain_factors","Lists factors that cannot be confirmed from the available satellite observations, possible alternative explanations, or evidence needed for further assessment.",{"id":594,"name":595,"field":596,"intro":597,"type":587},7701,"Diagnostic Question","diagnostic_question","Asks about possible convective triggering mechanisms based on the satellite observation clues.",{"id":599,"name":600,"field":601,"intro":602,"type":587},7702,"Diagnostic Reasoning Process","diagnostic_reasoning","Explains how the time-series observation clues lead to a possible trigger mechanism and distinguishes observed facts from inferences.",{"id":604,"name":605,"field":606,"intro":607,"type":587},7703,"Observation-Supported Conclusions","supported_conclusions","Lists conclusions directly supported by the satellite observation clues and explains their evidential basis.",{"id":609,"name":610,"field":611,"intro":612,"type":587},7704,"Inferred Trigger Mechanism","inferred_trigger_mechanism","States a possible mechanism for newly developing convection based on the clues, without presenting the inference as a confirmed fact.",{"id":614,"name":615,"field":616,"intro":617,"type":587},7705,"Satellite Observation Clues","satellite_observation_clues","Describes time-series satellite observations, including cloud development, cloud-top cooling, and localized cloud expansion.",[619,623,627,631],{"id":620,"question":621,"answer":622},5682,"What does the dataset contain?","It covers satellite time-series clues such as cloud development, cooling cloud tops, and localized cloud expansion. Records include a diagnostic question, possible trigger mechanisms, observation-supported conclusions, unresolved factors, and the reasoning process.",{"id":624,"question":625,"answer":626},5683,"How does it distinguish observations from inferred mechanisms?","Records separate the observed clues, conclusions those clues support, and possible trigger mechanisms. They also identify uncertainties or alternative explanations so that an inference is not presented as an established fact.",{"id":628,"question":629,"answer":630},5684,"What are suitable use cases?","The dataset can support abductive reasoning research in meteorological satellite remote sensing, reasoning SFT, model evaluation, and prototyping diagnostic Q&A systems for convective initiation. Model outputs should be treated as analytical support and checked against other observations or expert judgment.",{"id":632,"question":633,"answer":634},5685,"How can I access the data, and what are the licensing terms?","Refer to the product page for the available download method, data format, and license terms. Before use, verify the permitted scope, attribution requirements, and whether commercial use is allowed; no specific license or file format is stated in this description.",[636,648,658],{"id":637,"relate_table":638,"relate_id":639,"file_size":573,"file_name":8,"path":8,"duration":573,"cate":483,"file_format":8,"audio_rate":8,"audio_channel":522,"audio_bit_depth":522,"quality":8,"annotation":640,"cate_name":641,"uncertain_factors":642,"diagnostic_question":643,"diagnostic_reasoning":644,"supported_conclusions":645,"inferred_trigger_mechanism":646,"satellite_observation_clues":647},14579,"union_cubo",866260232,"{\"uncertain_factors\": \"The imagery cannot determine whether the cloud elements shared an updraft, whether their outflows interacted, or whether a separate convergence zone was present. It also does not establish the environmental instability or vertical wind profile. Radar and wind observations, together with environmental profiles, would be needed to test the merger-related interpretation.\", \"diagnostic_question\": \"Does the rapid deepening near the junction of the two growing towers support a merger-related trigger, and what remains uncertain?\", \"diagnostic_reasoning\": \"The strongest observed cooling and expansion occurred near the point where the two cloud elements became contiguous, making interaction between them a reasonable hypothesis. The sequence supports localized deepening near that junction. It does not directly show the dynamical process, so a merger-related trigger remains an inference rather than an observed fact.\", \"supported_conclusions\": \"Two nearby cloud towers grew, their visible cloud edges became contiguous, and a localized cloud-top region near their junction expanded and cooled rapidly. The surrounding cloud shield changed less over the same interval. These observations establish spatial and temporal association, not the cause of the deepening.\", \"inferred_trigger_mechanism\": \"Enhanced ascent associated with the interaction or apparent merger of the two cloud elements is a plausible trigger for the localized deepening. The close timing and location support considering this mechanism, but satellite cloud fields alone cannot establish the underlying airflow or confirm that two distinct updrafts merged.\", \"satellite_observation_clues\": \"From 16:20 to 16:50 UTC, visible imagery shows two compact cumulus towers about 12 km apart. Both enlarge, and their cloud edges become contiguous by 16:38 UTC. A single brighter, broader cloud-top region is apparent near their junction by 16:45 UTC. Infrared brightness temperature in that region falls from approximately −21°C at 16:30 UTC to −49°C at 16:50 UTC; the surrounding cloud shield expands only slightly.\"}","文本","The imagery cannot determine whether the cloud elements shared an updraft, whether their outflows interacted, or whether a separate convergence zone was present. It also does not establish the environmental instability or vertical wind profile. Radar and wind observations, together with environmental profiles, would be needed to test the merger-related interpretation.","Does the rapid deepening near the junction of the two growing towers support a merger-related trigger, and what remains uncertain?","The strongest observed cooling and expansion occurred near the point where the two cloud elements became contiguous, making interaction between them a reasonable hypothesis. The sequence supports localized deepening near that junction. It does not directly show the dynamical process, so a merger-related trigger remains an inference rather than an observed fact.","Two nearby cloud towers grew, their visible cloud edges became contiguous, and a localized cloud-top region near their junction expanded and cooled rapidly. The surrounding cloud shield changed less over the same interval. These observations establish spatial and temporal association, not the cause of the deepening.","Enhanced ascent associated with the interaction or apparent merger of the two cloud elements is a plausible trigger for the localized deepening. The close timing and location support considering this mechanism, but satellite cloud fields alone cannot establish the underlying airflow or confirm that two distinct updrafts merged.","From 16:20 to 16:50 UTC, visible imagery shows two compact cumulus towers about 12 km apart. Both enlarge, and their cloud edges become contiguous by 16:38 UTC. A single brighter, broader cloud-top region is apparent near their junction by 16:45 UTC. Infrared brightness temperature in that region falls from approximately −21°C at 16:30 UTC to −49°C at 16:50 UTC; the surrounding cloud shield expands only slightly.",{"id":649,"relate_table":638,"relate_id":650,"file_size":573,"file_name":8,"path":8,"duration":573,"cate":483,"file_format":8,"audio_rate":8,"audio_channel":522,"audio_bit_depth":522,"quality":8,"annotation":651,"cate_name":641,"uncertain_factors":652,"diagnostic_question":653,"diagnostic_reasoning":654,"supported_conclusions":655,"inferred_trigger_mechanism":656,"satellite_observation_clues":657},14578,755555194,"{\"uncertain_factors\": \"The imagery does not provide direct measurements of the near-surface wind, the location or strength of a sea-breeze front, or atmospheric stability. A larger-scale wind shift or another boundary could produce a similar cloud pattern. Surface wind observations and environmental profiles would be needed to evaluate these alternatives.\", \"diagnostic_question\": \"Could the inland progression and localized cloud-top cooling indicate sea-breeze-related initiation, and what can be concluded from the satellite sequence alone?\", \"diagnostic_reasoning\": \"The inland movement of the cloud line and the growth of a cell along its inland edge make a coastal circulation a plausible trigger hypothesis. The cooling brightness temperature supports rapid cloud-top development, not the identity of the forcing. Because the sequence contains no direct wind or stability measurements, the sea-breeze interpretation should remain tentative.\", \"supported_conclusions\": \"The cloud line formed and progressed inland during the observed period. A cell on its inland edge grew and cooled rapidly at cloud top, while the offshore cloud field changed little. The sequence supports localized convective development associated in time and location with the inland-moving cloud line.\", \"inferred_trigger_mechanism\": \"A sea-breeze-related convergence zone is a plausible explanation for the inland progression and localized strengthening. The spatial and temporal pattern is consistent with that mechanism, but it does not by itself confirm a sea breeze or rule out other sources of convergence.\", \"satellite_observation_clues\": \"Between 15:10 and 16:00 UTC, visible satellite imagery over a coastal sector shows a loose line of cumulus clouds forming about 15–25 km inland and advancing farther inland. One cell along the inland edge becomes distinctly larger between 15:35 and 15:55 UTC; its infrared brightness temperature decreases from approximately −16°C to −43°C. The adjacent offshore cloud field changes little during this period.\"}","The imagery does not provide direct measurements of the near-surface wind, the location or strength of a sea-breeze front, or atmospheric stability. A larger-scale wind shift or another boundary could produce a similar cloud pattern. Surface wind observations and environmental profiles would be needed to evaluate these alternatives.","Could the inland progression and localized cloud-top cooling indicate sea-breeze-related initiation, and what can be concluded from the satellite sequence alone?","The inland movement of the cloud line and the growth of a cell along its inland edge make a coastal circulation a plausible trigger hypothesis. The cooling brightness temperature supports rapid cloud-top development, not the identity of the forcing. Because the sequence contains no direct wind or stability measurements, the sea-breeze interpretation should remain tentative.","The cloud line formed and progressed inland during the observed period. A cell on its inland edge grew and cooled rapidly at cloud top, while the offshore cloud field changed little. The sequence supports localized convective development associated in time and location with the inland-moving cloud line.","A sea-breeze-related convergence zone is a plausible explanation for the inland progression and localized strengthening. The spatial and temporal pattern is consistent with that mechanism, but it does not by itself confirm a sea breeze or rule out other sources of convergence.","Between 15:10 and 16:00 UTC, visible satellite imagery over a coastal sector shows a loose line of cumulus clouds forming about 15–25 km inland and advancing farther inland. One cell along the inland edge becomes distinctly larger between 15:35 and 15:55 UTC; its infrared brightness temperature decreases from approximately −16°C to −43°C. The adjacent offshore cloud field changes little during this period.",{"id":659,"relate_table":638,"relate_id":660,"file_size":573,"file_name":8,"path":8,"duration":573,"cate":483,"file_format":8,"audio_rate":8,"audio_channel":522,"audio_bit_depth":522,"quality":8,"annotation":661,"cate_name":641,"uncertain_factors":662,"diagnostic_question":663,"diagnostic_reasoning":664,"supported_conclusions":665,"inferred_trigger_mechanism":666,"satellite_observation_clues":667},14577,1110755957,"{\"uncertain_factors\": \"The imagery alone does not establish low-level wind convergence, an outflow boundary, or the thermodynamic state of the air feeding the tower. Differential surface heating or another environmental forcing could also be involved. Wind observations, radar data, and environmental profiles would help distinguish these possibilities.\", \"diagnostic_question\": \"What trigger mechanism is most consistent with the rapid development of the tower at the cloud-field edge, and which parts of that interpretation are supported by the imagery?\", \"diagnostic_reasoning\": \"The rapid area increase and falling infrared brightness temperature indicate that the tower was deepening during the observed interval. Its position at the edge of the broader cloud field makes an interaction near that interface a reasonable hypothesis. However, cloud-top evolution does not directly measure low-level airflow, so the evidence supports the development pattern more strongly than any specific dynamical trigger.\", \"supported_conclusions\": \"A localized cloud element expanded substantially and its infrared brightness temperature decreased over roughly 30 minutes. Its development occurred at the edge of the broader cloud field, while nearby elements changed less. These are the direct temporal and spatial observations in the record.\", \"inferred_trigger_mechanism\": \"Localized convergence near the interface between the growing tower and the broader cloud field is a plausible trigger. The timing and location are consistent with an interaction at that interface, but the imagery does not directly establish convergence or identify its cause.\", \"satellite_observation_clues\": \"From 14:05 to 14:35 UTC, visible imagery shows a compact cumulus tower developing along the eastern edge of a broader, nearly stationary cloud field. Its apparent cloud area increases from about 10 to 28 km². Over the same interval, the tower's infrared brightness temperature falls from approximately −19°C to −47°C, while nearby cloud elements show little comparable change.\"}","The imagery alone does not establish low-level wind convergence, an outflow boundary, or the thermodynamic state of the air feeding the tower. Differential surface heating or another environmental forcing could also be involved. Wind observations, radar data, and environmental profiles would help distinguish these possibilities.","What trigger mechanism is most consistent with the rapid development of the tower at the cloud-field edge, and which parts of that interpretation are supported by the imagery?","The rapid area increase and falling infrared brightness temperature indicate that the tower was deepening during the observed interval. Its position at the edge of the broader cloud field makes an interaction near that interface a reasonable hypothesis. However, cloud-top evolution does not directly measure low-level airflow, so the evidence supports the development pattern more strongly than any specific dynamical trigger.","A localized cloud element expanded substantially and its infrared brightness temperature decreased over roughly 30 minutes. Its development occurred at the edge of the broader cloud field, while nearby elements changed less. These are the direct temporal and spatial observations in the record.","Localized convergence near the interface between the growing tower and the broader cloud field is a plausible trigger. The timing and location are consistent with an interaction at that interface, but the imagery does not directly establish convergence or identify its cause.","From 14:05 to 14:35 UTC, visible imagery shows a compact cumulus tower developing along the eastern edge of a broader, nearly stationary cloud field. Its apparent cloud area increases from about 10 to 28 km². Over the same interval, the tower's infrared brightness temperature falls from approximately −19°C to −47°C, while nearby cloud elements show little comparable change.","{\"uncertain_factors\":\"The imagery cannot determine whether the cloud elements shared an updraft, whether their outflows interacted, or whether a separate convergence zone was present. It also does not establish the environmental instability or vertical wind profile. Radar and wind observations, together with environmental profiles, would be needed to test the merger-related interpretation.\",\"diagnostic_question\":\"Does the rapid deepening near the junction of the two growing towers support a merger-related trigger, and what remains uncertain?\",\"diagnostic_reasoning\":\"The strongest observed cooling and expansion occurred near the point where the two cloud elements became contiguous, making interaction between them a reasonable hypothesis. The sequence supports localized deepening near that junction. It does not directly show the dynamical process, so a merger-related trigger remains an inference rather than an observed fact.\",\"supported_conclusions\":\"Two nearby cloud towers grew, their visible cloud edges became contiguous, and a localized cloud-top region near their junction expanded and cooled rapidly. The surrounding cloud shield changed less over the same interval. These observations establish spatial and temporal association, not the cause of the deepening.\",\"inferred_trigger_mechanism\":\"Enhanced ascent associated with the interaction or apparent merger of the two cloud elements is a plausible trigger for the localized deepening. The close timing and location support considering this mechanism, but satellite cloud fields alone cannot establish the underlying airflow or confirm that two distinct updrafts merged.\",\"satellite_observation_clues\":\"From 16:20 to 16:50 UTC, visible imagery shows two compact cumulus towers about 12 km apart. Both enlarge, and their cloud edges become contiguous by 16:38 UTC. A single brighter, broader cloud-top region is apparent near their junction by 16:45 UTC. Infrared brightness temperature in that region falls from approximately −21°C at 16:30 UTC to −49°C at 16:50 UTC; the surrounding cloud shield expands only slightly.\"}","MOBIUSI INC","https:\u002F\u002Fstatic.mobiusi.com\u002Fmobiwusi\u002F20250829\u002F7bf4ac62b4533e2b809998a6f1c5491e.png?Expires=1792463130&OSSAccessKeyId=LTAI5tH8MQqhgeiAtrzCHrxM&Signature=v6Tr8jBrdm4s5wU1SnnyGsYg%2Bhw%3D&x-oss-process=image%2Fresize%2Cm_fill%2Cw_35%2Ch_35",[672,678],{"type":673,"title":674,"count_data":675},"bar","Length distribution",[676],{"name":677,"value":483},"1k lower",{"type":679,"title":680,"count_data":681},"pie","Language distribution",[682],{"name":683,"value":483},"English"]