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ความย่อ
Stratospheric water vapor 1% increase. 30% may be due to increased methane.
Observations using balloon-borne frost-point hygrometers, have detected an approximately 1% per year increase in stratospheric water vapor at Boulder, Colorado, since 1980. Besides implications for climate change, increased water vapor can affect the rate of chemical ozone loss, for example, by increasing the incidence of polar stratospheric clouds. Satellite measurements of water vapor, although not of adequate length for accurate trend determination, suggest that the increase may extend to other latitudes.
Observations have provided evidence for a widespread increase in stratospheric water vapor, which plays a role both in cooling the lower stratosphere and in depleting ozone through chemical interactions, thereby contributing to climate processes. However, the water vapor trends are not fully defined, nor are their cause understood.
Stratospheric water vapor measurements at a single location (Boulder, Colorado, U.S., 40°N) for the period 1981-2000 show a statistically significant increase of approximately 1%/year over altitudes 15-28 km. For the shorter period 1991-2001, global satellite measurements covering latitudes 60°N-60°S show a similar trend of 0.6-0.8%/year for altitudes ~25-50 km, but no significant trend at lower altitudes. The increases in water vapor are substantially larger than can be explained by tropospheric methane trends. Characterization of stratospheric water vapor trends is limited by the lack of global long-term measurements.
References
. Archived from the original on 10/16/2004. Retrieved on 10/02/2009.
== Summary == Stratospheric water vapor 1% increase. 30% may be due to increased methane. * Observations using balloon-borne frost-point hygrometers, have detected an approximately 1% per year
ไฟล, bams, climate, assess, boulder, water, vapor, 2002, ไฟล, ประว, ไฟล, หน, าท, ภาพน, การใช, ไฟล, วนกลางไม, ภาพท, รายละเอ, ยดส, งกว, าน, bams, climate, assess, boulder, water, vapor, 2002, 8206, กเซล, ขนาดไฟล, โลไบต, ชน, ดไมม, image, ปภาพหร, อไฟล, เส, ยงน, นฉ. ifl prawtiifl hnathimiphaphni karichiflswnklangimmiphaphthimiraylaexiydsungkwani BAMS climate assess boulder water vapor 2002 png 8206 775 425 phikesl khnadifl 9 kiolibt chnidimm image png rupphaphhruxiflesiyngni tnchbbxyuthi khxmmxns raylaexiyddanlang epnkhxkhwamthiaesdngphlcak ifltnchbbinkhxmmxns khxmmxnsepnewbistinokhrngkarsahrbekbrwbrwmsuxesri thi khunsamarthchwyid phaphkrafni khwrcathuksrangihmepnkrafiksewketxr sungmikhxdixikhlayprakar duephimetimthikhxmmxns suxtxngkarekbkwadsahrbsarsnethsephimetim hakphaphnimiinrupaebbkrafiksewketxrxyuaelw krunaxpohldaelaaethnthiaemaebbnidwy vector version available i chuxphaphihm i aenanaepnxyangyingihtngchuxiflewketxrihmnninrupaebb BAMS climate assess boulder water vapor 2002 svg aelwisaemaebb Vector version available hrux Vva sungimtxngichpharamietxr chuxphaphihmkhwamyx Stratospheric water vapor 1 increase 30 may be due to increased methane Observations using balloon borne frost point hygrometers have detected an approximately 1 per year increase in stratospheric water vapor at Boulder Colorado since 1980 Besides implications for climate change increased water vapor can affect the rate of chemical ozone loss for example by increasing the incidence of polar stratospheric clouds Satellite measurements of water vapor although not of adequate length for accurate trend determination suggest that the increase may extend to other latitudes 1 2 Observations have provided evidence for a widespread increase in stratospheric water vapor which plays a role both in cooling the lower stratosphere and in depleting ozone through chemical interactions thereby contributing to climate processes However the water vapor trends are not fully defined nor are their cause understood 3 Stratospheric water vapor measurements at a single location Boulder Colorado U S 40 N for the period 1981 2000 show a statistically significant increase of approximately 1 year over altitudes 15 28 km For the shorter period 1991 2001 global satellite measurements covering latitudes 60 N 60 S show a similar trend of 0 6 0 8 year for altitudes 25 50 km but no significant trend at lower altitudes The increases in water vapor are substantially larger than can be explained by tropospheric methane trends Characterization of stratospheric water vapor trends is limited by the lack of global long term measurements 3 References Ozone Depletion Archived from the original on 10 16 2004 Retrieved on 10 02 2009 http www esrl noaa gov gmd publications annrpt24 416 htm a b http www al noaa gov WWWHD pubdocs assessment02 executive summary html no longer available karxnuyatichsiththi Public domain Public domain false falseThis image is in the public domain because it contains materials that originally came from the U S National Oceanic and Atmospheric Administration taken or made as part of an employee s official duties العربي ة cestina Deutsch Zazaki English espanol eesti suomi francais magyar italiano 日本語 한국어 makedonski മലയ ള Plattduutsch Nederlands polski portugues romană russkij sicilianu slovenscina Turkce tiếng Việt 中文 中文 简体 Source http www cmdl noaa gov hotitems watervapor html prawtiifl khlikwnthi ewlaephuxduiflthipraktinkhnann wnthi ewlarupyxkhnadphuichkhwamehn pccubn20 04 20 emsayn 2550775 425 9 kiolibt Toomuchcash Summary Stratospheric water vapor 1 increase 30 may be due to increased methane Observations using balloon borne frost point hygrometers have detected an approximately 1 per year hnathimiphaphni hnatxipni oyngmathiphaphni aekseruxnkrack karichiflswnklang wikixuntxipniichiflni karichbn ar wikipedia org غازات دفيئة karichbn bg wikipedia org Parnikov gaz karichbn el wikipedia org Aeria toy 8ermokhpioy karichbn en wikipedia org Greenhouse gas karichbn gu wikipedia org ગ ર નહ ઉસ વ ય karichbn he wikipedia org גז חממה karichbn pt wikipedia org Gases do efeito estufa Usuario CaveatLector2022 Gases do efeito estufa karichbn ro wikipedia org Gaz cu efect de seră karichbn ta wikipedia org ப ங க ட ல வள மம karichbn te wikipedia org గ ర న హ స వ య వ ekhathungcak https th wikipedia org wiki ifl BAMS climate assess boulder water vapor 2002 png, wikipedia, วิกิ หนังสือ, หนังสือ, ห้องสมุด,
