Showing posts with label Paleoclimatology. Show all posts
Showing posts with label Paleoclimatology. Show all posts

Sunday, March 23, 2014

Marcott et al (2013)

A study by Marcott et al that reconstructed the Earth’s climate over the past 11,300 years using data gathered by various proxies at 73 locations globally. The findings of this study showed that the Earth had been gradually cooling over the past 5,000 years up until about 100 years ago, when it began to warm. The Holocene era, the studied time period, experienced gradual climate changes which allowed for the flora and fauna to adjust. The more recent changes though, are more rapid and may exceed the hottest period during the Holocene period. The recent warming is due to human activity, not natural causes. This is evident especially when examining the fact that because of the Earth’s orientation, the Norther Hemisphere should be experiencing cool summers as part of a cooling trend, which is not occurring. It is projected that the temperature will increased anywhere from 2 degrees to 11.5 degrees Fahrenheit by the end of this century.  
Three key findings of the study include the fact that the 1.3 degree cooling that occurred over the last 5,000 years was reversed in just the past 100 years, and the temperature will continue to rapidly increase. Another key finding is that with the natural changes of the Earth the Northern Hemisphere was projected to experience intense cooling over the next few thousand years but most likely will not because of the increase output levels of carbon dioxide and continued warming. A third finding is that this past century is an anomaly because we have not experienced this level of warming since the most recent ice age over 11,000 years ago.

marcott-et-al-2013-2.jpg

Figure 1: Temperature Anomaly for previous 2,000 and 11,000 years.
These two graphs temperature data for the Earth over the Holocene period. The figure on the left shows the same data as the figure on the right, zoomed in to 2,000 years. These graphs illustrate the warming and gradual cooling experienced during the Holocene period with the rapid jump in temperature over the past 100 years. As illustrated in the graph on the right, the current temperature is very close to the warmest time of the Holocene period.


According the Michael Mann of Pennsylvania State University, the main conclusion of this study by Marcott et al is “the rate of warming appears to be unprecedented as far back as the authors are able to go (to the boundary with the last ice age). And the rate of warming appears to have no analog in the past”. The warming that we are experiencing, and the rate at which it is occurring is not by means of nature as it has been in the past. With increased human activity and output of carbon dioxide among other greenhouse gases into the environment, the Earth is going through rapid changes that we have not seen before.
Concerns that Robert Rohde, the chief data analyst behind the Berkeley Earth Surface Temperature project, has are that in the study they relied too heavily on their proxy data which was spread out in time. This can blur or obscure the fluctuations in the data. Because of this he thinks that, “we can’t use the analysis of Marcott et al. to draw any firm conclusions about how unique the rapid changes of the twentieth century are compared to the previous 10,000 years.” Ultimately he recognizes the impact that the findings have in building upon current knowledge as well as assisting in future studies, but he urges the use of caution when comparing their findings and current events.
According to Richard Alley, of Pennsylvania State University, the big-picture messages from this study are, for one, “Our high assessed confidence that the recent warming is mostly human-driven, and that the costs will become large if the warming becomes large, do not primarily rest on how much warmer or colder today is than some particular time in the past, or even on how fast the recent changes are relative to those in the past.” Meaning scientists aren’t conducting these studies and saying that because today is hotter than it was 1,000 years ago means that we’re experiencing global warming; they look at the many factors that go into what climate is and what the climate is and has been around the world. Another takeaway is, “Whether the past was naturally warmer or cooler than recently, and whether the changes were faster or slower than recently, are of great interest to climate scientists in learning how the climate system works, including the strength of feedbacks.” So while we cannot look at 1 day or 1 year for comparison, it is still extremely important and valuable that scientists continue to study the past in attempts to understand how climate works that that we may appropriately prepare for the future.
Roger Pielke, professor at the University of Colorado, addresses in a blog post that the media made some mistakes when covering this study. There has been various coverage of the study that explains the resulting temperature data as fitting into the “hockey stick” analogy. The coverage explains that there has been a sharp increase in temperature in the past 100 years, the blade of the stick. Pielke explains this is wrong. He explains that the 20th century data is “not statistically robust” therefore there can be no “blade” for Marcott et al’s study.    

Tuesday, March 4, 2014

Ice Cores

Because ice cores clearly show different layers of ice, dust, volcanic ash, etc, years and seasons are clearly distinguishable. This means that scientists can zero in on different years fairly easily and analyze what was happening during that time. Ice cores reveal atmospheric circulation patterns, because they show dust, volcanic ash, salts, etc. This means that scientists can analyze what they find in the ice cores in order to see what was happening but also why. They are able to determine wind strengths and pressure centers from the concentration of dust, ash, salt, etc. Ice cores also hold information about carbon dioxide concentrations. From the concentration of carbon dioxide in a particular part of the ice core, scientists can determine if that part of the Earth was experiencing a glacial or interglacial period because lower concentrations correlate with colder temperatures and visa versa.


Figure 1: Ice Core Data
Image Source: http://joannenova.com.au/globalwarming/graphs/ice-cores/vostok-ice-core-petit-web.gif

This figure shows the relationship between carbon dioxide concentrations found in ice cores in Antarctica as well as the temperatures. Seeing this correlation, scientists can now further relate lower concentrations with colder temperatures and high concentrations of carbon dioxide with high temperatures. 

Ocean Sediments Profile

Here I have created a mock dating profile for Ocean Sediments. In includes a little bit about ocean sediments as well as it's strengths, weaknesses, "goal" as well as two figures.

Thursday, February 27, 2014

Dendroclimatology

Dendroclimatology is the process of using tree rings to determine the past climate of the Earth. Scientists look at width to determine if the climate then fostered favorable conditions for growth. Scientists also looked at density, which can give better data than ring width. Tree rings have many advantages as climate proxies. Because tree’s have rings that are consistent markers of time, it is fairly easy to get precise dates. Furthermore, because tree rings respond to more than just temperature, they can be used to determine other aspects of past climate as well. Scientists collect tree rings, often using a handheld device, before bringing it into a lab to study and test. Scientists are able to determine things such as droughts, volcanic eruptions, and of course temperature.
To read more check out the wikipedia page here or this interesting case study!

What is Paleoclimatology?

Paleoclimatology is the study of the Earth’s past climates. While we have temperature records for several decades into the past, the Earth has been around and thriving for millions of years. Before we had thermometers and other measures to collect data about our climate, there was no way of recording temperature, weather, or climate. Thankfully, scientists have been able to obtain proxy records (approximate records of climate) from the Earth itself. By examining tree rings, ice cores, coral reefs, and the sediment at the bottom of bodies of water scientists can find out a lot about what was happening on the Earth thousands of years ago. Holli riebeek related paleoclimatology to a crime scene and how detectives put clues and pieces of evidence together (Paleoclimatology: Introduction, 2005). Scientists take clues from what they discover about the past and piece together the Earth’s past climate.
Why would we want to know about the Earth’s climate thousands of years ago? Knowing about the past and how the Earth has experienced climate previously is instrumental in figuring out where our Earth is headed in the future. Climate change is happening, fast, and by looking into the past scientists are able to see if there are trends, or patterns that we may be falling into. It can also help us estimate how much of human activity is effecting climate change, and how much could be just natural.

To read all of Holli Riebeek’s Paleoclimatology: Introduction click here!

Wednesday, February 26, 2014

Ray Bradley

After reading Ray Bradley’s transcription of a lecture given in 2009, these are two questions that I would ask him if I could, and why.
Because of the ways in which data is collected (ice cores, tree rings, reefs, lakes) are there areas of the world that do not have that kind of data (data that looks back thousands of years)? For example, in deserts, how is/could data be collected there?
  • I would hope that he would explain where in the world there are deficits of data and why. I also would expect him to say whether or not there is a way to collect data in those places, and why they have yet to do so. I want to know if this is something that scientists are concern about or think about, or if they think that they have all this data collection under control. Do they think that they’re getting information from enough of a variety of places? I think a scientist’s perspective on this is the most important, because it is their work.
Scientists have all this information about the ways in which our climate is changing, and we know that there needs to be some switches away from coal as an energy source, but what can I do? What can someone who isn’t a political figure or millionaire do to help protect the Earth against global warming?

  • I can’t say that I have any idea what he would say in response to this. After learning about what he is describing, I want to know how I can productively use this information. I want to know his answer because knowing all this is well and good, but if I can’t do anything by myself, I want to at least know how to help get this information out there.

Diatom Algae Populations

In this video we see scientists collect diatoms from lakes and examining the sediments at the bottom of the lake. Because of the nature of the diatoms they examine, they are able to see which diatoms were present in the past. Using diatoms as a tool, they are able to see how climate change and global warming affect lake ecosystems, including the surrounding plant life.
To see the video click here!

"How Do We Know?"

This video features different scientists describing the different ways we can reconstruct climate history. Some of the things they talk about are coral reef cores, sediment layers in a lake basin, ice cores, and deep sea sediments. With all these kinds of data collection, scientists can reconstruct a decent amount the Earth’s past climates.
To watch the video click here!

Ice Core Records

In this video, Richard Alley shows us how examining ice can show us about what happened on this Earth thousands of years ago. Scientists can analyze the gases, especially carbon dioxide, present in the ice to figure how much carbon dioxide was in the atmosphere at that time. Over time they’ve been able to see how the levels of carbon dioxide correspond very closely with the temperatures of that time. Their relationship is not something to be ignored.
To watch the video click here!