询问Google

您搜索了: nocturnal emission (英语 - 他加禄语)

人工翻译

来自专业的译者、企业、网页和免费的翻译库。

添加一条翻译

英语

他加禄语

信息

英语

nocturnal emission

他加禄语

Pagpapalabas ng gabi

最后更新: 2017-08-31
使用频率: 1
质量:

参考: 匿名

英语

emission

他加禄语

paglabas

最后更新: 2018-06-13
使用频率: 1
质量:

参考: 匿名

英语

nocturnal

他加禄语

panggabi

最后更新: 2013-10-19
使用频率: 1
质量:

参考: 匿名

英语

carbon emission

他加禄语

paglabas ng carbon

最后更新: 2020-01-24
使用频率: 1
质量:

参考: 匿名

英语

nocturnal person

他加禄语

panggabi na tao

最后更新: 2019-01-04
使用频率: 1
质量:

参考: 匿名

英语

emission of water

他加禄语

paglabas

最后更新: 2016-02-28
使用频率: 1
质量:

参考: 匿名

英语

synonym of nocturnal

他加禄语

dumarapo

最后更新: 2019-09-25
使用频率: 1
质量:

参考: 匿名

英语

emission of semen

他加禄语

nilabasan ng tamod

最后更新: 2017-04-23
使用频率: 1
质量:

参考: 匿名

英语

the word emission means

他加禄语

Emmision

最后更新: 2020-12-11
使用频率: 1
质量:

参考: 匿名

英语

smoke emission from factory

他加禄语

Maitim na usok galing tambutyo

最后更新: 2019-09-04
使用频率: 1
质量:

参考: 匿名

英语

Climate change includes both the global warming driven by human emissions of greenhouse gases, and the resulting large-scale shifts in weather patterns.[1] Though there have been previous periods of climatic change, since the mid-20th century the rate of human impact on Earth's climate system and the global scale of that impact have been unprecedented.[2] That human activity has caused climate change is not disputed by any scientific body of national or international standing.[3] The largest driver has been the emission of greenhouse gases, of which more than 90% are carbon dioxide (CO 2) and methane.[4] Fossil fuel burning for energy consumption is the main source of these emissions, with additional contributions from agriculture, deforestation, and industrial processes.[5] Temperature rise is accelerated or tempered by climate feedbacks, such as loss of sunlight-reflecting snow and ice cover, increased water vapour (a greenhouse gas itself), and changes to land and ocean carbon sinks. Observed temperature from NASA versus the 1850–1900 average as a pre-industrial baseline. The main driver for increased global temperatures in the industrial era is human activity, with natural forces adding variability.[6] Because land surfaces heat faster than ocean surfaces, deserts are expanding and heat waves and wildfires are more common.[7] Surface temperature rise is greatest in the Arctic, where it has contributed to melting permafrost, and the retreat of glaciers and sea ice.[8] Increasing atmospheric energy and rates of evaporation cause more intense storms and weather extremes, which damage infrastructure and agriculture.[9] Rising temperatures are limiting ocean productivity and harming fish stocks in most parts of the globe.[10] Current and anticipated effects from undernutrition, heat stress and disease have led the World Health Organization to declare climate change the greatest threat to global health in the 21st century.[11] Environmental effects include the extinction or relocation of many species as their ecosystems change, most immediately in coral reefs, mountains, and the Arctic.[12] Even if efforts to minimize future warming are successful, some effects will continue for centuries, including rising sea levels, rising ocean temperatures, and ocean acidification from elevated levels of CO 2.[13] Some effects of climate change Ecological collapse possibilities. Bleaching has damaged the Great Barrier Reef and threatens reefs worldwide. Many of these effects are already observed at the current level of warming, which is about 1.1 °C (2.0 °F).[15] The Intergovernmental Panel on Climate Change (IPCC) has issued a series of reports that project significant increases in these impacts as warming continues to 1.5 °C (2.7 °F) and beyond.[16] Under the Paris Agreement, nations agreed to keep warming "well under 2.0 °C (3.6 °F)" by reducing greenhouse gas emissions. However, under those pledges, global warming would reach about 2.8 °C (5.0 °F) by the end of the century, and current policies will result in about 3.0 °C (5.4 °F) of warming.[17] Limiting warming to 1.5 °C (2.7 °F) would require halving emissions by 2030, then reaching near-zero levels by 2050.[18] Mitigation efforts include the research, development, and deployment of low-carbon energy technologies, enhanced energy efficiency, policies to reduce fossil fuel emissions, reforestation, and forest preservation. Climate engineering techniques, most prominently solar radiation management and carbon dioxide removal, have substantial limitations and carry large uncertainties. Societies and governments are also working to adapt to current and future global-warming effects through improved coastline protection, better disaster management, and the development of more resistant crops.

他加禄语

Climate change includes both the global warming driven by human emissions of greenhouse gases, and the resulting large-scale shifts in weather patterns.[1] Though there have been previous periods of climatic change, since the mid-20th century the rate of human impact on Earth's climate system and the global scale of that impact have been unprecedented.[2] That human activity has caused climate change is not disputed by any scientific body of national or international standing.[3] The largest driver has been the emission of greenhouse gases, of which more than 90% are carbon dioxide (CO 2) and methane.[4] Fossil fuel burning for energy consumption is the main source of these emissions, with additional contributions from agriculture, deforestation, and industrial processes.[5] Temperature rise is accelerated or tempered by climate feedbacks, such as loss of sunlight-reflecting snow and ice cover, increased water vapour (a greenhouse gas itself), and changes to land and ocean carbon sinks. Observed temperature from NASA versus the 1850–1900 average as a pre-industrial baseline. The main driver for increased global temperatures in the industrial era is human activity, with natural forces adding variability.[6] Because land surfaces heat faster than ocean surfaces, deserts are expanding and heat waves and wildfires are more common.[7] Surface temperature rise is greatest in the Arctic, where it has contributed to melting permafrost, and the retreat of glaciers and sea ice.[8] Increasing atmospheric energy and rates of evaporation cause more intense storms and weather extremes, which damage infrastructure and agriculture.[9] Rising temperatures are limiting ocean productivity and harming fish stocks in most parts of the globe.[10] Current and anticipated effects from undernutrition, heat stress and disease have led the World Health Organization to declare climate change the greatest threat to global health in the 21st century.[11] Environmental effects include the extinction or relocation of many species as their ecosystems change, most immediately in coral reefs, mountains, and the Arctic.[12] Even if efforts to minimize future warming are successful, some effects will continue for centuries, including rising sea levels, rising ocean temperatures, and ocean acidification from elevated levels of CO 2.[13] Some effects of climate change Ecological collapse possibilities. Bleaching has damaged the Great Barrier Reef and threatens reefs worldwide. Many of these effects are already observed at the current level of warming, which is about 1.1 °C (2.0 °F).[15] The Intergovernmental Panel on Climate Change (IPCC) has issued a series of reports that project significant increases in these impacts as warming continues to 1.5 °C (2.7 °F) and beyond.[16] Under the Paris Agreement, nations agreed to keep warming ng.[17] Limiting warming to 1.5 °C (2.7 °F) would require halving emissions by 2030, then reaching near-zero levels by 2050.[18] Mitigation efforts include the research, development, and deployment of low-carbon energy technologies, enhanced energy efficiency, policies to reduce fossil fuel emissions, reforestation, and forest preservation. Climate engineering techniques, most prominently solar radiation management and carbon dioxide removal, have substantial limitations and carry large uncertainties. Societies and governments are also working to adapt to current and future global-warming effects through improved coastline protection, better ps.

最后更新: 2020-11-23
使用频率: 1
质量:

参考: 匿名
警告:包含不可见的HTML格式

英语

Climate change includes both the global warming driven by human emissions of greenhouse gases, and the resulting large-scale shifts in weather patterns.[1] Though there have been previous periods of climatic change, since the mid-20th century the rate of human impact on Earth's climate system and the global scale of that impact have been unprecedented.[2] That human activity has caused climate change is not disputed by any scientific body of national or international standing.[3] The largest driver has been the emission of greenhouse gases, of which more than 90% are carbon dioxide (CO 2) and methane.[4] Fossil fuel burning for energy consumption is the main source of these emissions, with additional contributions from agriculture, deforestation, and industrial processes.[5] Temperature rise is accelerated or tempered by climate feedbacks, such as loss of sunlight-reflecting snow and ice cover, increased water vapour (a greenhouse gas itself), and changes to land and ocean carbon sinks. Observed temperature from NASA versus the 1850–1900 average as a pre-industrial baseline. The main driver for increased global temperatures in the industrial era is human activity, with natural forces adding variability.[6] Because land surfaces heat faster than ocean surfaces, deserts are expanding and heat waves and wildfires are more common.[7] Surface temperature rise is greatest in the Arctic, where it has contributed to melting permafrost, and the retreat of glaciers and sea ice.[8] Increasing atmospheric energy and rates of evaporation cause more intense storms and weather extremes, which damage infrastructure and agriculture.[9] Rising temperatures are limiting ocean productivity and harming fish stocks in most parts of the globe.[10] Current and anticipated effects from undernutrition, heat stress and disease have led the World Health Organization to declare climate change the greatest threat to global health in the 21st century.[11] Environmental effects include the extinction or relocation of many species as their ecosystems change, most immediately in coral reefs, mountains, and the Arctic.[12] Even if efforts to minimize future warming are successful, some effects will continue for centuries, including rising sea levels, rising ocean temperatures, and ocean acidification from elevated levels of CO 2.[13] Some effects of climate change Ecological collapse possibilities. Bleaching has damaged the Great Barrier Reef and threatens reefs worldwide. Many of these effects are already observed at the current level of warming, which is about 1.1 °C (2.0 °F).[15] The Intergovernmental Panel on Climate Change (IPCC) has issued a series of reports that project significant increases in these impacts as warming continues to 1.5 °C (2.7 °F) and beyond.[16] Under the Paris Agreement, nations agreed to keep warming "well under 2.0 °C (3.6 °F)" by reducing greenhouse gas emissions. However, under those pledges, global warming would reach about 2.8 °C (5.0 °F) by the end of the century, and current policies will result in about 3.0 °C (5.4 °F) of warming.[17] Limiting warming to 1.5 °C (2.7 °F) would require halving emissions by 2030, then reaching near-zero levels by 2050.[18] Mitigation efforts include the research, development, and deployment of low-carbon energy technologies, enhanced energy efficiency, policies to reduce fossil fuel emissions, reforestation, and forest preservation. Climate engineering techniques, most prominently solar radiation management and carbon dioxide removal, have substantial limitations and carry large uncertainties. Societies and governments are also working to adapt to current and future global-warming effects through improved coastline protection, better disaster management, and the development of more resistant crops.

他加禄语

Climate change includes both the global warming driven by human emissions of greenhouse gases, and the resulting large-scale shifts in weather patterns.[1] Though there have been previous periods of climatic change, since the mid-20th century the rate of human impact on Earth's climate system and the global scale of that impact have been unprecedented.[2] That human activity has caused climate change is not disputed by any scientific body of national or international standing.[3] The largest driver has been the emission of greenhouse gases, of which more than 90% are carbon dioxide (CO 2) and methane.[4] Fossil fuel burning for energy consumption is the main source of these emissions, with additional contributions from agriculture, deforestation, and industrial processes.[5] Temperature rise is accelerated or tempered by climate feedbacks, such as loss of sunlight-reflecting snow and ice cover, increased water vapour (a greenhouse gas itself), and changes to land and ocean carbon sinks. Observed temperature from NASA versus the 1850–1900 average as a pre-industrial baseline. The main driver for increased global temperatures in the industrial era is human activity, with natural forces adding variability.[6] Because land surfaces heat faster than ocean surfaces, deserts are expanding and heat waves and wildfires are more common.[7] Surface temperature rise is greatest in the Arctic, where it has contributed to melting permafrost, and the retreat of glaciers and sea ice.[8] Increasing atmospheric energy and rates of evaporation cause more intense storms and weather extremes, which damage infrastructure and agriculture.[9] Rising temperatures are limiting ocean productivity and harming fish stocks in most parts of the globe.[10] Current and anticipated effects from undernutrition, heat stress and disease have led the World Health Organization to declare climate change the greatest threat to global health in the 21st century.[11] Environmental effects include the extinction or relocation of many species as their ecosystems change, most immediately in coral reefs, mountains, and the Arctic.[12] Even if efforts to minimize future warming are successful, some effects will continue for centuries, including rising sea levels, rising ocean temperatures, and ocean acidification from elevated levels of CO 2.[13] Some effects of climate change Ecological collapse possibilities. Bleaching has damaged the Great Barrier Reef and threatens reefs worldwide. Many of these effects are already observed at the current level of warming, which is about 1.1 °C (2.0 °F).[15] The Intergovernmental Panel on Climate Change (IPCC) has issued a series of reports that project significant increases in these impacts as warming continues to 1.5 °C (2.7 °F) and beyond.[16] Under the Paris Agreement, nations agreed to keep warming "well under 2.0 °C (3.6 °F)" by reducing greenhouse gas emissions. However, under those pledges, global warming would reach about 2.8 °C (5.0 °F) by the end of the century, and current policies will result in about 3.0 °C (5.4 °F) of warming.[17] Limiting warming to 1.5 °C (2.7 °F) would require halving emissions by 2030, then reaching near-zero levels by 2050.[18] Mitigation efforts include the research, development, and deployment of low-carbon energy technologies, enhanced energy efficiency, policies to reduce fossil fuel emissions, reforestation, and forest preservation. Climate engineering techniques, most prominently solar radiation management and carbon dioxide removal, have substantial limitations and carry large uncertainties. Societies and governments are also working to adapt to current and future global-warming effects through improved coastline protection, better disaster management, and the development of more resistant crops.

最后更新: 2020-11-23
使用频率: 1
质量:

参考: 匿名
警告:包含不可见的HTML格式

英语

Due to reduced travel and closures of heavy industry, there has been a decrease in air pollution and carbon emissions.

他加禄语

Dahil sa nabawasang paglalakbay at pagsara ng mabibigat na industriya, nabawasan ang polusyon sa hangin at paglabas ng carbon.

最后更新: 2020-08-25
使用频率: 1
质量:

参考: 匿名

英语

harmful emissions

他加禄语

paglabas

最后更新: 2015-10-07
使用频率: 1
质量:

参考: 匿名

获取更好的翻译,从
4,401,923,520 条人工翻译中汲取

用户现在正在寻求帮助:



Cookie 讓我們提供服務。利用此服務即表示你同意我們使用Cookie。 更多資訊。 確認