Vostok Ice core report

Balog was once a skeptic of climate change as he believed that the theory surrounding global warming was based off of computer models. Furthermore, he did not believe that humans could alter the world’s climate on such a global scale. However, through studies of ice records, long tubes of ice drilled from the ground, Balog found key evidence suggesting ideas contrary to his prior beliefs. These glacial tubes preserved historical records of the past similar to the rings of a tree, recording past temperatures and CO2 levels. Using these records, one can see the direct variation between temperature and CO2. Additionally, the recent spike in both

The Great Warming by Brian Fagan claims that environmental changes (most commonly prolonged droughts, El Niños, and La Niñas during the Medieval Warm Period) affect human civilization, including human’s trading abilities, overall movement, and quality of life. He examines the world’s ancient climate warming, known as the Medieval Warming, between the 10th and the 15th centuries, also mentioning the preceding and succeeding centuries. Fagan gathers his research using studies conducted by archaeologists, historians, and paleoclimatologists. Throughout his book, he refers to direct methods to study climate change, such as instrument records and historical documents, and indirect methods, such as ice, deep sea cores, coral records, and tree rings. Fagan digs into the rise and fall of multiple civilizations around the world as an effect of The Medieval Warming Period. As well as examining civilizations across the world, he attempts to connect the climate change patterns during The Medieval Warming Period to the current global warming faced today. The Great Warming discusses positive and negative connections between climate change and human civilizations across the world, starting in Europe and working its way into Asia, North America, South America, Africa, and even covering the arctic ice caps; however, throughout the book, Fagan has a hard time connecting his various ideas back to one main topic and can easily stray from his point about the effects of climate change.

Economic growth is vital to sustain human life; however, the unsustainable consumption of natural resources to attain this demand is leading to self-destruction. The Earth is facing environmental changes, including climate changes, which are altering the Earth system. Significantly higher thermal expansion is inescapable if the increasing pollution by carbon dioxide emission continues relentlessly. One evidence of this change is global warming and its impact in the Arctic Ice. The critical role of the Arctic in the global climate system implies that Arctic Ice changes will have far-reaching connotations for, and feedbacks to, the entire Earth. Currently, the warning signs include: rapid diminishing of sea ice, increased mass

A climate interval from around 1300 to 1750, with beginning and ending dates varying by geography (Wolfe, 2014), the Little Ice Age was a period of time in which mean annual temperatures decreased by about 0.6C and mountain glaciers expanded across the Northern Hemisphere. This period of time occurred after the Medieval Warm Period, around the Middle Ages, and is followed by the current period of warming (Rafferty & Jackson, 2016). This idea of climate cycles—known as Milankovitch cycles—shows that climate change is not a new phenomenon.

Climate change is evident throughout the world and is a major issue. It is no secret that our planet is getting warmer. Global warming is now recognized in the scientific community as a real problem. There are multiple aspects that are causing this issue. Majority of the warming is caused by greenhouse gases. Volcanic eruptions and changes in the intensity of solar radiation have offset the warming partially. It is estimated that average annual temperatures will increase 3.5°F-9.5°F by the century’s end.

Throughout history climates have drastically changed. There have been shifts from warm climates to the Ice Ages (Cunningham & Cunningham, 2009, p.204). Evidence suggests there have been at least a dozen abrupt climate changes throughout the history of the earth. There are a few suspected reasons for these past climate changes. One reason may be that asteroids hitting the earth and volcanic eruptions caused some of them. A further assumption is that 22-year solar magnetic cycles and 11-year sunspot cycles played a part in the changes. A further possibility is that a regular shifting in the angle of the moon orbiting earth causing changing tides and atmospheric circulation affects the global climate (Cunningham & Cunningham, 2009,

The report concludes, again with “high confidence”, that anthropogenic (human caused) warming has had a discernible influence on many of our planets physical and biological systems. While there are limitations and gaps in the knowledge available, particularly from undeveloped countries, the knowledge available allowed the group to attribute most of the observed increase in the globally averaged temperature since the mid-20th century to the observed increase in anthropogenic greenhouse gas concentrations. The analysis was necessarily limited in the number of systems and locations considered. In addition, natural temperature variability is larger at the regional than at the global scale, thus affecting identification of changes due to external forcing and at the regional scale other factors such as land-use change and pollution, are an environmental

Human produced carbon dioxide mainly caused by the burning of natural resources and deforestation has caused the earth’s temperature to rise (Spahni). The carbon dioxide adds to a problem known as the greenhouse effect. Greenhouse effect is the building up of different gases in the earth’s atmosphere causing the earth’s temperature to rise. Consequently, the key players in the greenhouse effect are as follows: water vapor 36-70%, carbon dioxide 9-26%, methane 4-9%, and ozone 3-7% (Russel). Thus, to determine the amount of CO2 and other gases that have been in the atmosphere in the past, ice core samples are taken and examined. There are ice core samples taken from as far back as 650,000 years ago (Siegenthaler). There has

It has been observed through various researches that in the last century, average temperatures across the globe increased by over 1.3°F with an increase of more than two times in the Arctic. (Bates, Kundzewicz, Wu, & Palutikof, June 2008). The results of climate change can also be seen in changing precipitation patterns, increases in ocean temperatures, changes in the sea level, and acidity and melting of glaciers and sea ice (USEPA, 2014).

The second main “driver” of global temperature change is reflectivity. Changes in reflectivity affect how much energy enter Earth’s system. When the sunlight reaches Earth, it can be reflected or absorbed, and that depends on the Earth’s surface and atmosphere; light colors reflect the most sunlight, while dark colors absorb more sunlight. Albedo, the amount of solar radiation reflected from an object or surface, indicates the amount of sunlight reflected as a percentage. Earth has an albedo of about 30%, which means that 70% of the sunlight is absorbed (NRC, 2010). This is important because the sunlight absorbed warms the land, water and atmosphere. In the past, this can be seen in the melting of sea ice or increases in cloud cover.

Earth has experienced many episodes of dramatic climate changes with different periods in earth history. There have been periods during which the entire planet has been covered in ice and at another time it has been scorchingly hot and dry. In this regards, earth has experienced at least three major periods of long- term frigid climate and ice ages interspersed with periods of warm climate. The last glacial period which current glaciers are the result of it, occurring during the last years of Pleistocene, from approximately 110,000 to 10,000 years age (Clayton, 1997). Indeed, glaciers present sensitive indicators of climate change and global warming and by estimating and monitoring the dynamic evolution of these ice masses, several

The Medieval Warm Period (MWP) refers to a relatively warm period lasting from about the 10th to the 14th century.2 However, the initial evidence for the MWP was largely based on data3 gathered from Europe, and more recent analyses indicate that the MWP was not a global phenomenon. A number of reconstructions of millennium-scale global temperatures have indicated that the maximum globally averaged temperature during the MWP was not as extreme as present-day temperatures and that the warming was regional rather than global. Perhaps the most well-known of these is that of Michael Mann and colleagues (Nature, 392, 1998, pg. 779). Their reconstruction produced the so-called “hockey stick” graphic that contributed to this conclusion in the 2001 assessment of the Intergovernmental Panel on Climate Change: “The…'Medieval Warm Period' appear(s) to have limited utility in describing trends in hemispheric or global mean temperature changes in past centuries." The accuracy of the “hockey stick” graphic was widely discussed in the press when the Mann et al. methodology was criticized by McIntyre and McKitrick (Geophys. Res. Lettr, 32, 2005, pg. L03710). Less attention was given to subsequent studies, such as that of Moberg and colleagues (Nature, 433, 2005, pg. 613) and Osborn and Briffa (Science, 311, 2006, pg. 841) that were based on different, independent methodologies but reached conclusions similar to Mann. Observations of melting high altitude glaciers are

This report focuses on an event that occurred a long time ago, known as the Little Ice Age. A description of what it is, how it began, how long it lasted, whether it was instantaneous or consistent over time, and how it is related to climate change are included in this paper. What the cause for the Little Ice Age and its effects and impact on society in the past, present, and future are discussed. Furthermore, the positive and negative feedback loops part of the Little Ice Age are addressed, and any future projections of an event similar to this are also talked about. Finally, a drawing of the various interactions between the event and each sphere of the Earth- the Hydrosphere, Biosphere, Lith¬osphere, Atmosphere- is included towards the end of the report. There are two interactions for each sphere. A conclusion wrapping all that was discussed in the report is encompassed within this paper. The Little Ice Age and its relation and impact on the climate and the Earth System are the major focus of this report.

Just in the last 650,000 years there have been seven cycles of glacial advance and retreat, with the abrupt end of the last ice age about 7,000 years ago marking the beginning of the modern climate era — and of human civilization. Earth-orbiting satellites and other technological advances have enabled scientists to see the big picture, collecting many different types of information about our planet and its climate on a global scale. This body of data, collected over many years, reveals the signals of a changing climate.

Scientists have discovered 'climate forcing’s ' influence variations in climate systems and based on the depth and period of such forcing’s the adjustments to climate may be in a shorter or longer earth cycle. Natural forcing’s like variations in earth 's orbit, solar variation, volcanic eruptions and motion of tectonic plates have influence on the Earth 's climate