Posts

Climate Change - Glacial archaeology

Image
Norway  is dotted with small glaciers, and 'permanent' snow patches . Around 7,000 years ago (5000 BC) the Earth was enjoying a warm climate: Then it cooled, allowing those icy areas to form. Now those glaciers and patches of perennial ice in the high mountains of Southern Norway have started to melt again, as the Earth is warming.  They contain all sorts of archaeological treasures. Anything from ancient shoes to 5000-year-old arrowheads.  As a result a new kind of archaeology has begun -  Glacial archaeology . In 2006,  an amateur archaeologist came across an amazingly well-preserved  ancient leather shoe  in   the Lendbreen ice patch in Norway.  When the shoe was examined and tested, archaeologists discovered the shoe was over 3,000 years old, and dated from the  Bronze Age . "Actually we should be slowly approaching a new ice age.  But in the past 20 years we have witnessed artefacts turning up in summer from in...

Climate Change - Ocean acidification - what does it mean?

Image
The phrase ' ocean acidification ' means that the  pH of seawater  is falling. The  pH scale  is used by scientists to describe  strength  of acids and alkalis.  Sea water  normally had a pH around 8.2  It has now reduced to 8.1, and will continue to reduce, as more CO 2  is added to the air by human activities. Some of the extra CO 2  in the air  dissolves  in the sea, and this affects sealife. Here is what one expert scientist has said about this - "A drop of 0.1-unit pH is equivalent to about a 26% increase in the ocean hydrogen ion concentration. "pH is likely to drop by 0.3-0.4 units by the end of the 21st century. "This will increase ocean hydrogen ion concentration (or acidity) by 100-150% above what it was in preindustrial times." Scott Doney, Senior Scientist, Woods Hole Oceanographic Institution, USA       Humanity's greenhouse gas emissions may be acidifying the oceans at a ...

Climate Change - Coal and carbon dioxide

Image
Coal, oil and natural gas are  fossil fuels . When they are burned, they  change the Earth's atmosphere. How is that possible?       C oal  is a good example. Coal was formed  hundreds of millions of years ago . Geologists say that a three-metre (10-foot) coal seam took between  12,000 and 60,000 years  to form . Ancient trees and other plants lived, died and were fossilised. All those plants took  carbon dioxide  out of the atmosphere.  Some larger coal seams are, for example, 10 metres thick. They took around  40,000 years to form,  but have been mined and burned in a little over  100 years. The fastest rise of CO 2  in the air seen in   the ice core record (800,000 years)  is  20 ppm in 1000 years. The CO 2  level in the atmosphere is now rising at around  20 ppm per decade . The  carbon  joins up with  oxygen  when it burns. Eac...

Climate Change - Carbon Sinks

Image
Carbon sinks  are natural systems that suck up and store  carbon dioxide  from the atmosphere. The main natural carbon sinks are  plants, the ocean and  soil.   Plants  grab carbon dioxide from the atmosphere to use in  photosynthesis ; some of this carbon is transferred to soil as plants die and decompose.  The  oceans  are a major carbon storage system for carbon dioxide.  Marine life also takes up the gas for photosynthesis, while some carbon dioxide simply dissolves in the seawater. 35 billion tonnes  of CO2 are produced each year by human activities. Currently, natural processes are absorbing about half of that. The figure of 33.4 billion metric tonnes of carbon dioxide is for 2010.   The remaining carbon dioxide is building up in the atmosphere.  

Climate Change - Corals and Coral Bleaching

Image
Healthy  coral  can be very colourful. Some coral reefs have started to look rather different. This is called ' coral bleaching '. To understand this, we need to start by looking at corals. Corals are animals that make a framework around them  that looks like rock. Coral animals ( polyps ) have tiny  plants -  algae  - living in their tissues. The algae provide food to the corals, which they produce by  photosynthesis . Reef-building corals only live in a limited temperature range. Like porridge, they should be 'not too hot and not too cold'. Coral reefs  are concentrated in a band around the equator, between 30 ° N and 30 ° S latitude. Algae in corals need light Corals grow in warm, clear, shallow waters that receive plenty of light. Most corals grow in the warmest water they can stand (about 85° F or 29° C).  This means that slight increases in ocean temperature can harm corals. High sea temperature is the main reas...

Climate Change - Russell Coope & the Discovery of Abrupt Climate Change

Image
Many people think climate change always happens slowly, but that is not the case......rather than hundreds, or thousands, of years, sometimes it can happen in decades. "Abrupt climate change"  was discovered by accident by Russell Coope (1930-2011), over 50 years ago. More recently he said: "We are  messing with the trigger  that causes climate change....the outcome is likely to be ferocious." In the 1950s, Russell Coope was a young geologist. He was studying layers of sediment formed during the  "Ice Ages" , a time geologists call the  Quaternary . He spotted something unusual in a quarry in the English Midlands.   This is his own description of what he found ... "I happened, entirely by accident, to visit a Quaternary gravel pit in which were exposed the spectacular bones of mammoth, woolly rhinoceros and bison.  Looking at their sediment matrix I was amazed to find enormous numbers of equally spectacular, if somewhat smaller, insec...

Climate Change - Is the Sun causing Global Warming? Or about to cause Global Cooling?

Image
It is often claimed that the  Sun  is causing global climate change. The Sun  is  the source of the heat on the Earth, but it has not suddenly become more active recently. The Sun may be going into a phase of lower activity - but that will not reverse global warming. When the Sun's energy arrives at the Earth, it travels through the air. Some is reflected back to space, but some hits the Earth and warms it. The warm Earth gives off  infrared radiation  with various wavelengths.   Some of those waves can pass back out of the air to space, but some are absorbed by certain gases in the air. The gases then re-emit the energy into the air. If there are more of those gases, less heat escapes into space, so the Earth warms. In the graph below, from the  Stanford Solar Center , carbon dioxide data comes from the Law Dome ice core in Antarctica, and from the observatory on Mauna Loa in Hawaii. The Earth has wa...