File:All palaeotemps.svg এই ফাইলের একটি ভেক্টর সংস্করণ। যখন উচ্চতর তখন এটি এই রাস্টার চিত্রের জায়গায় ব্যবহার করা উচিত। File:All palaeotemps.png → File:All palaeotemps.svg ভেক্টর গ্রাফিক্স সম্পর্কে আরও তথ্যের জন্য, কমন্স এসভিজিতে রূপান্তর সম্পর্কে পড়ুন। সেখানে মিডিয়াউইকির এসভিজি চিত্র সমর্থন সম্পর্কে তথ্য রয়েছে। উন্নত বিকল্প Alemannisch ∙ Bahasa Indonesia ∙ Bahasa Melayu ∙ British English ∙ català ∙ čeština ∙ dansk ∙ Deutsch ∙ eesti ∙ English ∙ español ∙ Esperanto ∙ euskara ∙ français ∙ Frysk ∙ galego ∙ hrvatski ∙ Ido ∙ italiano ∙ lietuvių ∙ magyar ∙ Nederlands ∙ norsk bokmål ∙ norsk nynorsk ∙ occitan ∙ Plattdüütsch ∙ polski ∙ português ∙ português do Brasil ∙ română ∙ Scots ∙ sicilianu ∙ slovenčina ∙ slovenščina ∙ suomi ∙ svenska ∙ Tiếng Việt ∙ Türkçe ∙ vèneto ∙ Ελληνικά ∙ беларуская (тарашкевіца) ∙ български ∙ македонски ∙ нохчийн ∙ русский ∙ српски / srpski ∙ татарча/tatarça ∙ українська ∙ ქართული ∙ հայերեն ∙ বাংলা ∙ தமிழ் ∙ മലയാളം ∙ ไทย ∙ 한국어 ∙ 日本語 ∙ 简体中文 ∙ 繁體中文 ∙ עברית ∙ العربية ∙ فارسی ∙ +/−

 

সারাংশ

This shows estimates of earth's global average surface air temperature over the ~540 My of the Phanerozoic Eon, since the first major proliferation of complex life forms on our planet. A substantial achievement of the last 30 years of climate science has been the production of a large set of actual measurements of temperature history (from physical proxies), replacing much of the earlier geological induction (i.e. informed guesses). The graph shows selected proxy temperature estimates, which are detailed below.

Because many proxy temperature reconstructions indicate local, not global, temperature -- or ocean, not air, temperature -- substantial approximation may be involved in deriving these global temperature estimates. As a result, the relativities of some of the plotted estimates are approximate, particularly the early ones.

Time scale

Time is plotted forward to the present, taken as 2015 CE. It joins five separate linearly scaled segments, expanding by about an order of magnitude at each vertical break. The breaks are not evenly distributed; rather they are positioned at geologically relevant times, which might be misleading since the break in the last interglacial makes it seem much longer:

• At the Mesozoic – Cenozoic boundary, ~65 My ago. This is the "K-T" boundary (now called "Cretaceous–Paleogene"), at which the dinosaurs became extinct.
• At the Miocene – Pliocene boundary, ~5.3 My ago.
• One million years ago, near the onset of the current, 100,000 year-dominated, glaciation cycle (previous glaciations were shorter).
• Near the last glacial maximum, 20,000 years ago.

Temperature scale

Surface air temperature is plotted as anomalies (differences) from the average over the reference interval 1960–1990 (which is about 14°C / 57°F), in both Celsius (left) and Fahrenheit (right).

Data

Panel 1: 540 to 65 million years ago

The panel 1 data is from stable oxygen isotope measurements from the shells of macroscopic marine organisms, collected by Veizer et al (1999),^[1] as re-interpreted by Royer et al (2004).^[2] The graph effectively reproduces the upper panel of Royer et al's figure 4, but with an expanded range (see below). The orange band shows the effect of extreme assumptions in application of the GEOCARB reconstruction to interpretation, and is not representative of the full uncertainly (which would be much larger).

Because the Royer and Veizer results are indicative of the temperature of the shallow tropical and subtropical seas where the organisms lived,^[2] they are unlikely to be fully representative of global average surface air temperature variation. The anomalies are plotted here expanded by a factor of two, as a very approximate conversion. Multiple confounding factors affect interpretation of samples this old, so panel 1 is best viewed as a qualitative indication of temperature (warmer/colder).^[3]

Panel 2: 65 to 5.3 million years ago

This data is from the Hansen et al (2013)^[4] interpretation of the global collection of oxygen isotope data from microscopic marine organisms of Zachos et al (2008).^[5]

This is a direct estimate of global average sea surface temperature, a close analogue of surface air temperature. Hansen et al describe it as a "first estimate", meaning an approximate one, but limited independent corroboration (e.g. Zachos et al (2006)^[6] for the Eocene optimum) indicates that it is substantially more quantitative than panel 1.

Panel 3: 5.3 to 1 million years ago

This data is from the Lisiecki and Raymo (2005)^[7][8] global stack of oxygen isotope data from microscopic marine organisms interpreted using the Hansen et al (2013)^[4] prescription.

At this scale, the Zachos et al stack (which also covers this interval) is virtually indistinguishable from the Lisiecki and Raymo stack. This is a direct estimate of global average sea surface temperature.

Panel 4: 1 million to 20,000 years ago

Two datasets are plotted:

1. Lisiecki and Raymo, as in panel 3.
2. Temperature estimates from stable hydrogen isotope measurements from the EPICA Dome C ice core from central Antarctica^[9] These temperature anomaly estimates are polar, not global, and are here divided by a standard polar amplification factor (2.0, as for example in Hansen et al (2013)^[4]) to approximately convert them to global estimates.

Panel 5: 20,000 years ago to present (2015)

Five datasets are plotted:

1. EPICA Dome C, as in panel 4.
2. Temperature estimates from oxygen isotope measurements on the north Greenland ice core, NGRIP,^[10] interpreted using the simple procedure of Johnsen et al (1989).^[11] (There are more modern and complex procedures which would yield slightly different interpretations.) Like the EPICA Dome C record, this record is polar, and is shown divided by a polar amplification factor of 2.0. The difference between this and dataset 1. illustrates the polar sea-saw hypothesis.
3. Global temperature estimates over the ~12,000 years of the Holocene from the multi-proxy collection and interpretation of Marcott et al (2013).^[12]
4. Instrumental (not proxy) data since 1850 from the Berkeley Earth project land-ocean dataset (2014),^[13] plotted as decadal means.
5. Projected temperatures for 2050 and 2100 from the IPCC Fifth Assessment Report's WG1 Summary for Policy Makers (2013)^[14] for the RCP8.5 scenario.

Open source

The Microsoft Excel spreadsheet that produced this image is available here: All_palaeotemps.xlsx. Retrieved on 3 May 2014..

References

See also

লাইসেন্স প্রদান

এই ফাইলটি ক্রিয়েটিভ কমন্স অ্যাট্রিবিউশন-শেয়ার অ্যালাইক ৩.০ আনপোর্টেড লাইসেন্সের আওতায় লাইসেন্সকৃত।

আপনি স্বাধীনভাবে:

• বণ্টন করতে পারেন – এ কাজটি অনুলিপি, বিতরণ এবং প্রেরণ করতে পারেন
• পুনঃমিশ্রণ করতে পারেন – কাজটি অভিযোজন করতে পারেন

নিম্নের শর্তাবলীর ভিত্তিতে:

• স্বীকৃতিপ্রদান – আপনাকে অবশ্যই যথাযথ স্বীকৃতি প্রদান করতে হবে, লাইসেন্সের একটি লিঙ্ক সরবরাহ করতে হবে এবং কোনো পরিবর্তন হয়েছে কিনা তা নির্দেশ করতে হবে। আপনি যেকোনো যুক্তিসঙ্গত পদ্ধতিতে এটি করতে পারেন। কিন্তু এমন ভাবে নয়, যাতে প্রকাশ পায় যে লাইসেন্সধারী আপনাকে বা আপনার এই ব্যবহারের জন্য অনুমোদন দিয়েছে।
• একইভাবে বণ্টন – আপনি যদি কাজটি পুনঃমিশ্রণ, রুপান্তর, বা এর ওপর ভিত্তি করে নতুন সৃষ্টিকর্ম তৈরি করেন, তবে আপনাকে অবশ্যই আপনার অবদান একই লাইসেন্স বা একই রকমের লাইসেন্সের আওতায় বিতরণ করতে হবে।

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