您搜索了: change is constant (英语 - 他加禄语)

change is the only constant in life
change is the only constant in life.

change is invtable
change is good

change, is the only constant thing in this world
ang pagbabago, ay ang tanging pare-pareho na bagay sa mundong ito

change is the only constantant thing in life
ang pagbabago ay ang nag-iisa lamang na pare-pareho sa buhay

ano ang ibig sabihin ng change is inevitable?
ano ang ibig sabihin ng pagbabago ay hindi maiiwasan?

change is the end result of all true learning
the roots of education are bitter, but the fruit is sweet

curriculum change is inevitable, necessary and desirable
curriculum change is inevitable, necessary and desirable

the clock of climate change is ticking in these magnificent landscapes.
ang orasan ng climate change ay kumikiliti sa magagandang landscapes.

work performance by associate joan palulan remained inconsistent. we have reached almost all the help but no change is seen.
work performance ni associate joan palulan ay nanatiling inconsistent.halos lahat na ng tulong ay naiabot na namin ngunit hindi nakikitaan ng pagbabago.

14 karat gold is only about 58% gold.however the mass density of a mixture with a particular composition is constant
14 kilatis ginto ay lamang tungkol sa 58% gold.however ang masa density ng isang timpla na may partikular na komposisyon ay pare-pareho

the list of changes is not available
ang talaan ng mga pagbabago ay wala

i think the teacher because the change is so big to my daughter and she learn a lot of good things i say my daughter be coming a ginue child
sa tingin ko ang guro dahil ang pagbabago ay napakalaki sa aking anak na babae at matututunan niya ang maraming magagandang bagay na sinasabi ko na ang aking anak na babae ay darating na isang matalinong bata

the continuity view says that change is gradual. children become more skillful in thinking, talking or acting much the same way as they get taller.
the continuity view says that change is gradual. children become more skillful in thinking, talking or acting much the same way as they get taller.

they are relatively permanent in their conten. the pattern roles and relations that enact in a particular culture become traditional and enduring although intitutions are subject to change is relatively slow
medyo permanente sila sa kanilang nilalaman

chemical change is a change of materials into another, new materials with different properties and one or more than one new substances are formed. it result when a substance combines with another to a new subtance
chemical change is a change of materials into another, new materials with different properties and one or more than one new substances are formed. it result when a substance combines with another to form a new subtance

the price change is reflected by the change in the quantity the consumer is willing to buy. this is shown by movement along the curve, because it is assumed that other factors do not change. only price influences the change in the quantity the consumer is willing to buy. this is why it is called single curve movement because each change is noticeable and contained in a single demand curve.
ang pagbabago ng presyo ay naipapakita ng pagbabago sa dami ng handang bilhin ng mamimili. ito a naipapakita sa paggalw sa iisang kurba (movement along the curve) ,sapagkat ipinalalagay na ang ibang salik ay hindi nagbabago. tanging ang presyo lamang ang nakakaimpluwensya sa pagbabago ng dami ng handang bilhin ng mamimili. kaya ito tinawag na paggalw sa iisang kurba dahil mapapansin na ang bawat pagbabago at nakapaloob sa iisang kurba ng demand.

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.
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.