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asoka the great

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他加禄语

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他加禄语

the great father

英语

great father

最后更新: 2022-06-14
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参考: 匿名

他加禄语

god is the great provider

英语

god your the great provider

最后更新: 2022-09-08
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参考: 匿名

他加禄语

talambuhay ni alexander the great

英语

talambuhay ni alexander the great

最后更新: 2023-12-04
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参考: 匿名

他加禄语

matter what the great idea was?

英语

does it matter what the great idea was?

最后更新: 2022-03-15
使用频率: 2
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参考: 匿名

他加禄语

sino si cyrus the great tagalog

英语

sino si cyrus the great tagalog

最后更新: 2020-12-06
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参考: 匿名

他加禄语

nothing beat's the great smile

英语

nothing beat's the great smile

最后更新: 2020-08-08
使用频率: 1
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参考: 匿名

他加禄语

ano ang katangian ni cyrus the great

英语

what is the nature of cyrus the great

最后更新: 2023-10-18
使用频率: 4
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参考: 匿名

他加禄语

don't be afraid to give up the good to go for the great.

英语

don't be afraid to give up the good to go for the great.

最后更新: 2020-09-29
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参考: 匿名

他加禄语

phone is the day that i feel better soon as i love you too dear friend and god bless u always been the most important thing that you lord for the great day

英语

playground slide

最后更新: 2021-02-14
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参考: 匿名

他加禄语

kaya siya ang napili ko dahil gusto ko yung isa sa mga works niya na "the great malayan" na kung saan kinuwento niya ang ang istorya ng buhay ng pambansang bayani natin na si jose rizal

英语

so he was the one i chose because i like one of his works "the great malayan" where he told the story of the life of our national hero jose rizal

最后更新: 2020-09-25
使用频率: 2
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参考: 匿名
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他加禄语

the bato national high school a place for the great and for the small the pride of common batohanons a partridge for the weak and for the strong our home to enjoy and to live in creator of happiness so fine our future to believe in alma mater we praise you all the time when we cry made it dry when we fall you lift so high we bring your name upon a pedestal he loyalty we have to bear everytime and every where a freind who loves forever more when we cry made it dry when we fall you lift s

英语

the bato national high school a place for the great and for the small the pride of common batohanons a partridge for the weak and for the strong our home to enjoy and to live in creator of happiness so fine our hope our future to believe in alma mater we praise you all the time when we cry made it dry when we fall you lift so high we bring your name upon a pedestal he loyalty we have to bear everytime and every where a freind who loves forever more when we cry made it dry when we fall you lift s

最后更新: 2024-02-13
使用频率: 2
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参考: 匿名

他加禄语

thank you letters are a great way to show appreciation for everything someone has done for you. a thank you letter from a student to their teacher can remind them of all the great memories and lessons you have shared together throughout the school year. thank you letters can also be a great way to show your teacher how much you appreciate all their hard work and dedication.

英语

thank you letters are a great way to show appreciation for everything someone has done for you. a thank you letter from a student to their teacher can remind them of all the great memories and lessons you have shared together throughout the school year. thank you letters can also be a great way to show your teacher how much you appreciate all their hard work and dedication.

最后更新: 2023-06-10
使用频率: 1
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参考: 匿名

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.

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.

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

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