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Tagalog

decreased gases in the atmosphere

Englisch

decreased gases in the atmosphere

Letzte Aktualisierung: 2021-04-24
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Tagalog

greenhouse gases at fossil fuels

Englisch

greenhouse gases and fossil fuels

Letzte Aktualisierung: 2016-08-16
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Tagalog

anong english nag transferred through gases

Englisch

because the weather is cold

Letzte Aktualisierung: 2021-05-14
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Tagalog

what objects or equipment causes excessive greenhouse gases?

Englisch

ano ang mga bagay o kagamitang nagiging sanhi ng labis na greenhouse gases?

Letzte Aktualisierung: 2017-02-01
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Tagalog

ano ang mga bagay o kagamitang nagiging sanhi ng labis na greenhouse gases?

Englisch

ano ang mga bagay o kagamitang nagiging sanhi ng labis na greenhouse gases?

Letzte Aktualisierung: 2017-02-01
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Tagalog

ang ice sheet ng greenland ay dumadanas ng greenhouse gases ibinubuga kung saan sa mundo.

Englisch

greenland's ice sheet suffers from greenhouse gases emitted elsewhere on earth.

Letzte Aktualisierung: 2016-10-27
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Tagalog

a layer of the greenhouse gases primarily water vapor and including much smaller amount of carbon dioxide methane and nitrous oxide acts as a thermal blanker of the earth absorbing heat and warming surface to alive supporting average

Englisch

i satellite observations reveal that the amount of spring snow cover in the northern hemisphere has decreased over the past five decided and that the snow is melting earlier

Letzte Aktualisierung: 2020-03-14
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Tagalog

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.

Englisch

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.

Letzte Aktualisierung: 2020-11-23
Nutzungshäufigkeit: 1
Qualität:

Referenz: Anonym
Warnung: Enthält unsichtbare HTML-Formatierung

Tagalog

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.

Englisch

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.

Letzte Aktualisierung: 2020-11-23
Nutzungshäufigkeit: 1
Qualität:

Referenz: Anonym
Warnung: Enthält unsichtbare HTML-Formatierung

Tagalog

limnic eruptions are a rare, but potentially deadly class of natural disaster, in which toxic gases are rapidly expelled from a saturated lake. the gas, in observed cases was carbon dioxide, which was unevenly distributed in the lake, causing part of the water to be saturated. volcanically active regions are particularly prone to this, as a eruptions may leave depressions for lakes to form in. once the lake is formed, volcanic gases, such a co2 or methane can seep into the water, and begin to accumulate in the cooler bottom waters, due to the higher saturation point than that of the warmer water above. this can also be the case when decaying organic matter is producing large amounts of gas. once this gradient is established, anything that disturbs the water can trigger a release of the gas, with disastrous effects on the surrounding environs. the dense cloud of released gas may stay low to the ground, being denser than normal air, and forming a poisonous fog.

Englisch

lithospherethe

Letzte Aktualisierung: 2017-02-18
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Referenz: Anonym

Tagalog

haligi 4 in talahanayan 4.4 nagpapakita kinatawan timbang densities sa ingles units. ito ay maaaring gamitin sa parehong paraan na mass densities ay used.one kagiliw-giliw na excercise ay upang makalkula ang bigat ng hangin sa kuwarto. (madalas ang mga tao ay hindi mapagtanto na hangin at iba pang mga gases ang mayroon timbang.)

Englisch

column 4 in table 4.4 shows representative weight densities in english units.these can be used in the same ways that mass densities are used.one interesting excercise is to compute the weight of the air in the room.(often people do not realize that air and other gases do have weight.)

Letzte Aktualisierung: 2016-08-06
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Tagalog

alerting employees and visitors in your facility to potentially flammable conditions is an important factor in reducing fires and injuries. whether you have dangerous gases in the area, flammable liquids, or simply need to remind people that no smoking is permitted in your facility, proper no smoking safety signs can be your first line of defense against serious accidents and injuries.

Englisch

no smoking signs picture

Letzte Aktualisierung: 2017-02-01
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