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Hofstra University : GEOL140: Paleoclimatology VOL. 21 doi:1029/2011GEOL1406873, 2011


Proposing the use of a global probe based network of durable
marine “laboratories” to quantify the global flux of
dimethylsulfide across the sea/air interface
S. LeoneA
A
Hofstra University Geology Department, Hempstead New York, USA

    Abstract
         As it stands now there are <1500 quality scientific papers written regarding the CLAW hypothesis,
    many of which confirm the hypothesis. The hypothesis was conceived by four scientists: R.J. Charlson, J.
    E. Lovelock, M. O. Andreae & S. G. Warren in a 1987 paper in Nature. The four last names of the
    scientists make the acronym CLAW. This hypothesis provides a fascinating concept that there is a
    complex interaction between marine organisms and the atmosphere that work together to oppose change in
    a particular system through a series of feedback loops. Phytoplankton in the ocean produces
    dymethylsulfide and dimethylsulphoniopropionate (DMS/DMSP). These substances act as cloud
    condensation nuclei (CCN). When there is an input of sunlight and an output of excessive phytoplankton,
    the DMS/DMSP is released into the atmosphere and facilitates the formation of clouds. The clouds
    increase albedo and cool the system. There is currently no consistent and unified global network of
    sensors to provide real time data regarding the production of DMS/DMSP. Most of the data collected
    regarding the concentrations and production of DMS/DMSP are from the Global Surface Sea water DMS
    database (http://saga.pmel.noaa.gov/dms), other databases, satellite information, and measurements made
    by individual researchers. The current collection of data is fairly accurate and is fit to be used in scientific
    writing. The general consensus though among climate scientists specializing in research pertaining to
    CLAW is that there needs to be a better data collection protocol and it needs to be implemented in a way
    that will facilitate quick and accurate data collection. For this reason I propose that there be a global
    network of renewably powered, remotely controlled “DMS laboratories” present in the ocean. The probes
    will utilize CalTech’s “lab on a chip” technology to gain accurate real-time data that will quantify the
    seawater DMS/DMSP distribution and its global flux across the sea/air interface.


    Background                                                      attacked his views. The Gaia hypothesis is a
                                                                    fairly controversial theory and its main critics
           Other planets in this solar system may                   purport that it verges on being a quasi religious
    have cores, and low-density atmospheres, but to                 belief and that it did not follow the reductionist
    the best of our knowledge, Earth is the only                    approach of modern science. Over the past 20
    planet that demonstrates such complex                           years the theory has begun to gain much wider
    interactions between the living organisms and                   acceptance among the scientific community
    their inorganic surroundings. This complex                      (Spowers 2000). Too lovelock though, it made
    interaction creates sets of self-regulating                     perfect sense, especially in light of the fact that
    phenomenon that sustain the life on Earth.                      he worked with NASA to find life on other
    Similar beliefs have been held by various                       planets. The stark contrast drawn between the
    indigenous cultures around the world throughout                 surface of planets like Venus and Mars
    history. The first western scientific model to                  compared to the surface of the earth allowed him
    describe this phenomenon was suggested by                       to realize just how incredible and unique our
    James Lovelock. His theory that identifies and                  planet actually is.
    attempts to quantify this global phenomenon is                          In a 2000 interview, Lovelock states that
    known as the Gaia Hypothesis (GH).                              other planets seemed to be in a state of
    Lovelock’s theory was inspired by his work with                 equilibrium. The atmospheres of planets like
    NASA developing technology to detect life on                    Mars and Venus are composed entirely of
    other planets. When he published his first paper                carbon dioxide. This indicates a lifeless state.
    on the topic in 1979, the scientific community                  Lovelock compares earths atmosphere to the gas
you put in your car. The rich mixture of oxygen      into the atmosphere, oxidizes to form a sulfate
and hydrocarbons is akin to the fuel going into      aerosol. This substance acts as a CCN. The
the intake manifold of a motor vehicle. The          reflectance or albedo of clouds is responsive to
atmosphere on Mars though is composed of             CCN density. Thus in turn the earth’s radiation
gasses akin to the exhaust of a car. From this he    budget is sensitive to the presence of DMS due
believes life on mars and Venus exhausted itself     to its impact on cloud formation. Regulation of
(Spowers 2000). This lead to the conclusion that     the climate can be achieved by the feedback that
the onset of global warming is a huge problem,       occurs through the effects of temperature and
in fact, in Lovelock’s opinion everything else is    sunlight on the populations of phytoplankton
secondary to the problems of rising levels of        and the production of DMS.
greenhouse gasses. He asserts that we are now                Oceanic phytoplankton, if pushed to
in a state of “positive feedback” and that instead   either extreme of their tolerance levels i.e. too
of mitigating the harm that is being done, the       hot and sunny or too cold and dim, will respond
system is “actually increasing so that as it         by varying their DMS emissions. This way they
warms, the systems are wiped out and the             can increase or decrease the insolation hitting
process speeds up.”(Spowers 2000). In essence,       the ocean surface by influencing the marine
treating this planet as a machine has gotten         cloud reflectivity. By doing this, phytoplankton
humans into a lot of trouble.          The Gaia      effectively drive the system back towards their
hypothesis helps us to see that nature can indeed    tolerance levels.
be seen as sacred and that there is still a lot we
don’t know. What we do know, though, is that
it’s important to assess the factors contributing
not only to the Gaia hypothesis but the entire
issue of climate change.
        Lovelock’s theory of Gaia is quite broad.
One of the main terrestrial phenomenons that
Lovelock and many others have studied in depth
that contributes great insight into Gaia is the
“CLAW Hypothesis.” The letters that spell the
word “CLAW” are taken from the names of the
scientists that wrote a 1987 article in Nature
(Lovelock et. al. 1987). Before the CLAW
hypothesis can be fully explored, it is important
to examine the role of clouds in the atmosphere.
The way that clouds affect the warming and
cooling of the earth is hard enough to quantify.
Understanding the way that clouds affect the
warming and cooling of the earth in a warming
world is an even bigger uncertainty. One of the
main forcing on cloud properties is the existence
and concentration of a cloud condensation nuclei
(CCN). A CCN is a tiny particle present in the            (Ayers et. al. 2007)
atmosphere that serves as a medium for the
nucleation of a water droplet that makes up a             DMS in the atmosphere comes from the
cloud.                                                ocean. When DMS is present in the ocean it is the
        The basis of the CLAW hypothesis is the       direct result of biological activity.
prospect that there are oceanic and atmospheric             Dymethylsulfoniopropionate (DMSP) is the
systems that are coupled in such a way that           precursor compound to DMS.             DMSP is
opposes changes in climate. In the ocean there        synthesized by phytoplankton and the amount of
are several thousand species of phytoplankton.        DMSP present depends on the species of
These phytoplankton produce a substance called        phytoplankton present. So far, direct emission of
dimethylsulfide (DMS). DMS, once released             DMS from phytoplankton has been observed in a
                                                      laboratory setting. It has not, however, been


                                                                                                         2
observed in the oceans. It is also likely that the          Once the DMSP is in the water, there are
action of grazing zooplankton and viruses have an       several processes that convert the substance into
affect on the phytoplankton community that yields       DMS. The complexity of the process is what is
substantial levels of DMSP in the water. It is          important to note for the purposes of this paper.
typical that the higher levels of DMSP and DMS          The early work in understanding the processes
usually correlate with the onset of a plankton          was based in physics and utilized different
bloom.                                                  variables pertaining to wind speed, solubility of
     In light of the fact that there has been no        DMS and other factors. Fully understanding the
direct observation of DMS/DMSP production in            complexities of the sea-air interface, knowing
phytoplankton in the oceans, it is important to         what we already know poses a significant
implement a system that will allow real time            challenge. A major difficulty in obtaining DMS
quantification of the levels of DMS/DMSP, the           measurements from the water is the wind speed
presence of viruses, the grazing zooplankton, the       associated with oceans experiencing large blooms.
temperature and sunlight concentration in a             The safety of scientists and observation platforms
particular location. A. Lana et. al. in their 2011      is a main concern and so until Ayers et. al. in
paper utilized state of the art climatological          1995 determined certain micrometeorological
records and interpolation/extrapolation techniques      techniques to gain a better understanding of this
to carry out their research. They identified several    flux. Still, the techniques are only predictions
significant issues with the current state of the        based on proxies of eddy accumulation and eddy
databases and individual measurements used for          covariance.
their research. There doesn’t seem to be any
quality control in the database and a lack of           Motivation:
unification of the DMS measurement protocol.                    The anthropogenic influence on the atmosphere
This is troubling to many for it retards any           is predicted to lead to significant changes global
research attempts regarding oceanic DMS/DMSP           climatic conditions. Roughly half of the current carbon
concentrations.                                        dioxide emissions are being absorbed by the ocean and
                                                       by land ecosystems. This absorption is sensitive to
     In addition to a lack of a unified measurement
                                                       climate as well as to atmospheric carbon dioxide
protocol, the role of DMSP or DMS in plankton          concentrations. This creates a feedback loop. (Cox et.
physiology is still unclear (Ayers et. al. 2007). It   al. 2000) The CLAW hypothesis though, has a
is hypothesized that the conversion of DMSP to         counterpart: the Anti-CLAW hypothesis. Lovelock
DMS may have something to do with relieving            contends that the constituents of the CLAW hypothesis
oxidative stress following exposure to UV              will reverse from their current state of negative feedback
radiation, nutrient limitation, or changes in          and wind up acting as a positive feedback loop
surface temperature. It has also been suggested        (Lovelock 2007). Considering the evidence of increased
that DMSP has osmoregulative properties or is a        atmospheric carbon presented by Cox et.al. and the fact
carrier in organic sulfur cycling. (S. M. Vallina      that as of now, there is a predicted increase in global
et. al. 2007)                                          temperature, it is likely that world oceans may
     The fact that the role of DMSP and DMS in         stratify.
                                                                   (Lovelock 2007)
plankton is unclear makes it difficult to
understand how the emission of DMSP or DMS
from plankton would change as the surface water
environment changed in response to climate
change. It would be important to know if
changing certain oceanic conditions would alter
the plankton community in such a way that would
promote species of plankton that were higher
emitters of DMSP or DMS. In addition it would
be of note to determine the extent to which
increasing acidity would have on phytoplankton
communities and their emission of DMSP, for
deformed plankton have been observed. (Norris
2003)


                                                                                                               3
This would reduce the supply of nutrients that up        energy back as outgoing long-wave (infrared)
well from the deep. These nutrients are key for the      radiation, also known as terrestrial radiation.
proper functioning of phytoplankton in its euphotic      Albedo is an important factor in the radiation
zone. In a CLAW hypothesis reversal, this would          balance, and clouds have the major effect on
lead to a decline in phytoplankton activity and thus     albedo. The optical properties of a cloud are a key
less DMS production. If there is less DMS present        issue to understanding and therefore predicting
in the atmosphere there will be less cloud               global climate change. A cloud's optical properties
formation and so less albedo. The problem with           are related to the size distribution and number of its
this is that the lack of cloud cover will potentially    droplets. The more cloud condensation nuclei, the
lead to further climate warming. This in turn, will      smaller the size of its water droplets and the higher
continue to reduce the global production of DMS.         the density of water droplets since the same
                                                         amount of water vapor is distributed among a
                                                         greater number of CCN. This affects the radiative
                                                         properties      (reflectance,    transmittance    and
                                                         absorbance) of the cloud. Because of the vast
                                                         amount of atmosphere between the sea and space,
                                                         there is a lot of room for cloud activity. When the
                                                         clouds are low and thick, they act as shields,
                                                         blocking and reflecting insolation into space. This
                                                         in turn cools the planet. When clouds are high up,
                                                         they can also trap the outgoing heat, which is in the
                                                         form of longwave radiation. This warms the
                                                         planet. On the whole, data suggests that clouds
                                                         have a general net cooling effect on the planet
                                                         (Norris 2003).
                                                                  Climate scientists have realized that
                                                         current models had a poor ability to accurately
                                                         reproduce the effect of clouds. For this reason,
                                                         scientists have made it a priority to measure and
                                                         understand more about clouds physical properties
                                                         and radiative fluxes. Programs like CERES, and
                                                         the IRI/LDEO Climate Data Library are observing
                                                         clouds from space in order to more accurately
                                                         quantify cloud properties and their respective effect
                                                         on albedo. If a more accurate model of cloud
                                                         physics can be expressed, scientists will be able to
                                                         construct more accurate simulations of climate
                                                         budget and projections of change. Based on what
                                                         we have learned over the years in regard to the
                                                         CLAW hypothesis, it is likely that DMS has an
         Having a global network of biosensors can       influence on the global heat budget and the
help keep scientists savvy to the changes occurring      hydrological cycle due to its impact on cloud
in real time.       The radiation balance has a          formation. In order to understand how any CLAW
fundamental effect on Earth's climate. About one         related feedback mechanism (positive or negative)
third of the solar radiation that reaches the Earth is   between the plankton population and the
reflected back into space by clouds and from earth       atmosphere might operate, it is vital that the
surfaces, such as ice and snow. The atmosphere           biological role of DMS/DMSP within the cells of
absorbs some solar energy, but most of the other         plankton is clarified. The reason for this is because
two thirds is absorbed by the land and oceans,           the biological role of DMS/DMSP in plankton is
which are warmed by the sunlight (Norris 2003).          inextricably tied to how the feedback between
The sun's energy is converted into heat, and the         biology and atmosphere may respond to
land and oceans then radiate a portion of this           environmental changes.           It seems that an


                                                                                                             4
understanding of this feedback process in the                      There will be an onboard computer with
CLAW hypothesis remains elusive (Ayers et. al.            power efficient processors capable of dynamically
2007). Being able to accurately quantify the              adjusting their frequencies to reduce energy
amount of DMS being produced in real time all             consumption. These chips will likely be akin to the
across the globe will be a vital contribution to the      A5 processing chips at the heart of Apple’s iPad’s
climate science community.                                and iPhones.          Because accurate location
         Currently, some of the most recent               quantification will be necessary, the units will be
research in the field has come from data contained        equipped with onboard GPS chips in order to
in the Global Surface Sea water DMS Database.             convey precise global coordinates at any time.
Simo et. Al. states that there is no quality control in             The super computer used for this research
the database. This was worth stressing because            will be a Cray XT system. Similar systems have
there doesn’t seem to be unification of the DMS           been installed at several operational meteorological
measurement        protocol,      and     very     few    and hydrological services and leading climate
intercalibration exercises have been conducted in         research centers worldwide. Examples include but
the last 30 years. Furthermore, a number of               are not limited too, NOAA, NCAR, Korea
sampling and analytical issues have been reported         Meteorological Administration (KMA), Brazilian
in recent years. For this reason it is important to       National Institute for Space Research (INPE) and
have a definitive, reliable, and long lasting network     Center for Weather Forecasts and Climate Studies
of instruments that provide real time analysis of the     (CPTEC), Danish Meteorological Institute (DMI),
DMS/DMSP sea and air measurements. This will              and the U.S. Naval Oceanographic Office
help to assess health of the planet based on the          (NAVO). (Nyberg 2010)
progression of cloud formation and earths radiation                In order for the unit to be able to
balance. In addition it will continue to support          communicate with the central data collection server
James Lovelock’s Gaia hypothesis.                         it will utilize very low frequency (VLF)
                                                          transmission to land based towers, which will then
  Proposal for new research                               be able to route the data to a server linked to a
         Using modified “lab on a chip” technology        super computer to analyze the collected data. The
developed by CalTech (Liu et. al. 2009) to                reason VLF transmissions were chosen as the
effectively create a network of interconnected,           transmission medium is because they are often
centrally linked “microlabs” to measure levels of         used in Integrated Communication Systems (ICS)
DMS and DMSP in phytoplankton on a global                 for naval vessels and HF ground-to-air
scale. The labs will be encapsulated in a specific        applications. The technology will likely come from
vessel designed for durability and ease of                Hagenuk Marinekommunikation (HMK). The
maintenance and potential retrofitting. The vessel        company has provided solutions for more than 25
will also be equipped with a propulsion system,           navies throughout the world who now rely on the
which draws energy from solar power, tidal                high level of technical expertise of HMK. Over
currents, or both. The unit will not only be able to      540 systems have been delivered for all classes of
run real time collection and transmission of DMS          ships, including 117 submarine systems.
and DMSP data, it will be able to determine the           Moreover, HMK provides a full service package
effects of CO2 concentrations, sunlight, grazing          including feasibility studies, system engineering,
zooplankton, temperature and viral lysis on the           hardware and software design, production, system
production, dissemination and oxidation of DMS            integration and setting to work as well as
and DMSP.                                                 integrated logistics combined with comprehensive
         In order to accomplish this, the unit will be    after sales services over the whole product life
equipped with several sensors, including but not          cycle. Lastly, the technology that allows user
limited too, a PH sensor, a thermometer, a                interface with the VLF system can be a single
photometer, a salt refractometer, a current speed         workstation that is expandable to a networking
sensor, and a heavy metal sensor. The unit will           multi-console client/server configuration that,
also be able to rise to the surface and extend a          according to the contractor, provides sophisticated
probe into the atmosphere in order to collect data        automated communications support for naval
regarding the concentrations of DMS/DMSP in the           applications. The solutions offered by HMK
air directly above a particular system.                   posses the reliability of a company providing for


                                                                                                            5
the United States navy, and the customizability         one phenomenon out of the trillions that exist on
necessary for such a specific application.              this planet, it is a step in the right direction.
           The communication ability of the units
  will boast two way transmission capabilities for      References
  the obvious purpose of relaying collected
  information back to the server, and the less          "Hagenuk Marinekommunikation - Naval VLF and SHF Radio
  obvious ability to receive remote course and                 Equipment."        Naval         Technology.     Hagenuk
                                                               Marinekommunikation. Web. 12 Dec. 2011.<http://www.naval-
  speed commands from a controlling computer.                  technology.com/contractors/navigation/hagenuk/>.
  This system would ideally be composed of
  several hundred of these units to create a global     Greg p. Ayers, Jill M. Cainey (2007) “The CLAW hypothesis: a review of
  network. Ideally a climate scientist would be                  the major developments”, Research Front, 4, 366-374
  able to identify one singular, or several units in
                                                        Lana, A, G Bell, R Simo, M Vallina, and L Bopp 2011"An updated
  one of the many strategically placed locations                climatology of surface dimethlysulfide concentrations and
  and have full control over the device(s). This                emission fluxes in the global ocean” Global Biogeochemical
  will allow for a level of accurate, real time                 Cycles. 25. 1-17.

  climatic data collection never before achieved.       Lovelock, James (2007).         The    Revenge    of   Gaia.    Penguin.
           The reason each unit has its own                     ISBN 0141025972.
  propulsion system, whether it be a set of             Mike Liu et. al. (2009) “Field Operational Sensor and Lab-on-a-Chip
  propellers or a series of pumps and jets is so the           System for Marine Environmental Monitoring and Analysis”
  units can maintain one fixed position in the sea,            CENS 1-3
  or move about the sea for however long a certain      Norris, Katina B. "Dimethylsulfide Emission: Climate Control by Marine
  experiment or research project dictates.                       Algae." CSA. ProQuest, Nov. 2003. Web. 12 Dec. 2011.
           An example of the novel application of                <http://www.csa.com/discoveryguides/dimethyl/overview.php>.

  this technology is the fact that so far there is no   Per Nyberg (2010) “Cray Supercomputers in Climate”, Weather and
  system of interconnected, un-tethered, real time             Ocean Modeling Cray 1-6
  data collecting mechanisms of this scale. There       Peter M. Cox, Richard A. Betts, Chris D. Jones, Steven A. Spall, & Ian J.
  have been global collaborations of many                        Totterdell (2000) “Acceleration of global warming due to
  different scientists and instrumental records, but             carbon-cycle feedbacks in a coupled climate model” Nature, 408,
                                                                 184-187
  the ingenuity behind this concept is to have one
  place for scientists to go to analyze the real time   R. J. Charlson, J. E. Lovelock, M. O. Andreae & S. G. Warren (1987)
  data of the DMS/DMSP concentrations and a                     “Oceanic phytoplankton, atmospheric sulphur, cloud albedo and
                                                                climate”, Nature, 326: 655-661
  other measurable factors in the marine climate
  system. The information can easily be archived        Rory Spowers (2000) “Interview: Living Planet” Geographical 25-27
  and made public for all scientists and individuals    S.M. Vallina, R. Simo, S. Gasso, C. de Boyer-Montegut et. al. (2007)
  who may not have the means to get to the                     “Analysis of a potential “solar radiation dose-dimethylsulfide-
  supercomputer that all the units are linked to.              cloud condensation nuclei” link from globally mapped seasonal
                                                               correlations” Global Biogeochemical Cycles, 21, 1-16
           Furthermore, the main goal of this global
  network is to have the ability to monitor the         Vallina, M, and R Simo. "What controls CCN seasonality in the Southern
  health of the planet. The possibility of the                   Ocean? A statistical analysis based on satellite-derived
                                                                 chlorophyll and CCN and model-estimated OH radical and
  oceanic feedback loop reversing and creating                   rainfall." Global Biogeochemical Cycles. 20. 1-13.
  another system that subjects this planet to
  unnecessary temperature increases is very real.
  James Lovelock is not the only scientist who is
  concerned with the future of our climate system.
  Although any scientist knows that the planet will
  survive long after humans are extinct, the focus
  of preventing climate change is to ensure the
  prosperity of humans and all other organic life
  alike. It is not farfetched that at some point the
  earth may shrug humans off its proverbial
  shoulder. This is why this proposal is so
  important. Although it is serving to quantify but


                                                                                                                              6

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Proposing the use of a global probe based network of durable marine “laboratories” to quantify the global flux of dimethylsulfide across the sea/air interface

  • 1. Hofstra University : GEOL140: Paleoclimatology VOL. 21 doi:1029/2011GEOL1406873, 2011 Proposing the use of a global probe based network of durable marine “laboratories” to quantify the global flux of dimethylsulfide across the sea/air interface S. LeoneA A Hofstra University Geology Department, Hempstead New York, USA Abstract As it stands now there are <1500 quality scientific papers written regarding the CLAW hypothesis, many of which confirm the hypothesis. The hypothesis was conceived by four scientists: R.J. Charlson, J. E. Lovelock, M. O. Andreae & S. G. Warren in a 1987 paper in Nature. The four last names of the scientists make the acronym CLAW. This hypothesis provides a fascinating concept that there is a complex interaction between marine organisms and the atmosphere that work together to oppose change in a particular system through a series of feedback loops. Phytoplankton in the ocean produces dymethylsulfide and dimethylsulphoniopropionate (DMS/DMSP). These substances act as cloud condensation nuclei (CCN). When there is an input of sunlight and an output of excessive phytoplankton, the DMS/DMSP is released into the atmosphere and facilitates the formation of clouds. The clouds increase albedo and cool the system. There is currently no consistent and unified global network of sensors to provide real time data regarding the production of DMS/DMSP. Most of the data collected regarding the concentrations and production of DMS/DMSP are from the Global Surface Sea water DMS database (http://saga.pmel.noaa.gov/dms), other databases, satellite information, and measurements made by individual researchers. The current collection of data is fairly accurate and is fit to be used in scientific writing. The general consensus though among climate scientists specializing in research pertaining to CLAW is that there needs to be a better data collection protocol and it needs to be implemented in a way that will facilitate quick and accurate data collection. For this reason I propose that there be a global network of renewably powered, remotely controlled “DMS laboratories” present in the ocean. The probes will utilize CalTech’s “lab on a chip” technology to gain accurate real-time data that will quantify the seawater DMS/DMSP distribution and its global flux across the sea/air interface. Background attacked his views. The Gaia hypothesis is a fairly controversial theory and its main critics Other planets in this solar system may purport that it verges on being a quasi religious have cores, and low-density atmospheres, but to belief and that it did not follow the reductionist the best of our knowledge, Earth is the only approach of modern science. Over the past 20 planet that demonstrates such complex years the theory has begun to gain much wider interactions between the living organisms and acceptance among the scientific community their inorganic surroundings. This complex (Spowers 2000). Too lovelock though, it made interaction creates sets of self-regulating perfect sense, especially in light of the fact that phenomenon that sustain the life on Earth. he worked with NASA to find life on other Similar beliefs have been held by various planets. The stark contrast drawn between the indigenous cultures around the world throughout surface of planets like Venus and Mars history. The first western scientific model to compared to the surface of the earth allowed him describe this phenomenon was suggested by to realize just how incredible and unique our James Lovelock. His theory that identifies and planet actually is. attempts to quantify this global phenomenon is In a 2000 interview, Lovelock states that known as the Gaia Hypothesis (GH). other planets seemed to be in a state of Lovelock’s theory was inspired by his work with equilibrium. The atmospheres of planets like NASA developing technology to detect life on Mars and Venus are composed entirely of other planets. When he published his first paper carbon dioxide. This indicates a lifeless state. on the topic in 1979, the scientific community Lovelock compares earths atmosphere to the gas
  • 2. you put in your car. The rich mixture of oxygen into the atmosphere, oxidizes to form a sulfate and hydrocarbons is akin to the fuel going into aerosol. This substance acts as a CCN. The the intake manifold of a motor vehicle. The reflectance or albedo of clouds is responsive to atmosphere on Mars though is composed of CCN density. Thus in turn the earth’s radiation gasses akin to the exhaust of a car. From this he budget is sensitive to the presence of DMS due believes life on mars and Venus exhausted itself to its impact on cloud formation. Regulation of (Spowers 2000). This lead to the conclusion that the climate can be achieved by the feedback that the onset of global warming is a huge problem, occurs through the effects of temperature and in fact, in Lovelock’s opinion everything else is sunlight on the populations of phytoplankton secondary to the problems of rising levels of and the production of DMS. greenhouse gasses. He asserts that we are now Oceanic phytoplankton, if pushed to in a state of “positive feedback” and that instead either extreme of their tolerance levels i.e. too of mitigating the harm that is being done, the hot and sunny or too cold and dim, will respond system is “actually increasing so that as it by varying their DMS emissions. This way they warms, the systems are wiped out and the can increase or decrease the insolation hitting process speeds up.”(Spowers 2000). In essence, the ocean surface by influencing the marine treating this planet as a machine has gotten cloud reflectivity. By doing this, phytoplankton humans into a lot of trouble. The Gaia effectively drive the system back towards their hypothesis helps us to see that nature can indeed tolerance levels. be seen as sacred and that there is still a lot we don’t know. What we do know, though, is that it’s important to assess the factors contributing not only to the Gaia hypothesis but the entire issue of climate change. Lovelock’s theory of Gaia is quite broad. One of the main terrestrial phenomenons that Lovelock and many others have studied in depth that contributes great insight into Gaia is the “CLAW Hypothesis.” The letters that spell the word “CLAW” are taken from the names of the scientists that wrote a 1987 article in Nature (Lovelock et. al. 1987). Before the CLAW hypothesis can be fully explored, it is important to examine the role of clouds in the atmosphere. The way that clouds affect the warming and cooling of the earth is hard enough to quantify. Understanding the way that clouds affect the warming and cooling of the earth in a warming world is an even bigger uncertainty. One of the main forcing on cloud properties is the existence and concentration of a cloud condensation nuclei (CCN). A CCN is a tiny particle present in the (Ayers et. al. 2007) atmosphere that serves as a medium for the nucleation of a water droplet that makes up a DMS in the atmosphere comes from the cloud. ocean. When DMS is present in the ocean it is the The basis of the CLAW hypothesis is the direct result of biological activity. prospect that there are oceanic and atmospheric Dymethylsulfoniopropionate (DMSP) is the systems that are coupled in such a way that precursor compound to DMS. DMSP is opposes changes in climate. In the ocean there synthesized by phytoplankton and the amount of are several thousand species of phytoplankton. DMSP present depends on the species of These phytoplankton produce a substance called phytoplankton present. So far, direct emission of dimethylsulfide (DMS). DMS, once released DMS from phytoplankton has been observed in a laboratory setting. It has not, however, been 2
  • 3. observed in the oceans. It is also likely that the Once the DMSP is in the water, there are action of grazing zooplankton and viruses have an several processes that convert the substance into affect on the phytoplankton community that yields DMS. The complexity of the process is what is substantial levels of DMSP in the water. It is important to note for the purposes of this paper. typical that the higher levels of DMSP and DMS The early work in understanding the processes usually correlate with the onset of a plankton was based in physics and utilized different bloom. variables pertaining to wind speed, solubility of In light of the fact that there has been no DMS and other factors. Fully understanding the direct observation of DMS/DMSP production in complexities of the sea-air interface, knowing phytoplankton in the oceans, it is important to what we already know poses a significant implement a system that will allow real time challenge. A major difficulty in obtaining DMS quantification of the levels of DMS/DMSP, the measurements from the water is the wind speed presence of viruses, the grazing zooplankton, the associated with oceans experiencing large blooms. temperature and sunlight concentration in a The safety of scientists and observation platforms particular location. A. Lana et. al. in their 2011 is a main concern and so until Ayers et. al. in paper utilized state of the art climatological 1995 determined certain micrometeorological records and interpolation/extrapolation techniques techniques to gain a better understanding of this to carry out their research. They identified several flux. Still, the techniques are only predictions significant issues with the current state of the based on proxies of eddy accumulation and eddy databases and individual measurements used for covariance. their research. There doesn’t seem to be any quality control in the database and a lack of Motivation: unification of the DMS measurement protocol. The anthropogenic influence on the atmosphere This is troubling to many for it retards any is predicted to lead to significant changes global research attempts regarding oceanic DMS/DMSP climatic conditions. Roughly half of the current carbon concentrations. dioxide emissions are being absorbed by the ocean and by land ecosystems. This absorption is sensitive to In addition to a lack of a unified measurement climate as well as to atmospheric carbon dioxide protocol, the role of DMSP or DMS in plankton concentrations. This creates a feedback loop. (Cox et. physiology is still unclear (Ayers et. al. 2007). It al. 2000) The CLAW hypothesis though, has a is hypothesized that the conversion of DMSP to counterpart: the Anti-CLAW hypothesis. Lovelock DMS may have something to do with relieving contends that the constituents of the CLAW hypothesis oxidative stress following exposure to UV will reverse from their current state of negative feedback radiation, nutrient limitation, or changes in and wind up acting as a positive feedback loop surface temperature. It has also been suggested (Lovelock 2007). Considering the evidence of increased that DMSP has osmoregulative properties or is a atmospheric carbon presented by Cox et.al. and the fact carrier in organic sulfur cycling. (S. M. Vallina that as of now, there is a predicted increase in global et. al. 2007) temperature, it is likely that world oceans may The fact that the role of DMSP and DMS in stratify. (Lovelock 2007) plankton is unclear makes it difficult to understand how the emission of DMSP or DMS from plankton would change as the surface water environment changed in response to climate change. It would be important to know if changing certain oceanic conditions would alter the plankton community in such a way that would promote species of plankton that were higher emitters of DMSP or DMS. In addition it would be of note to determine the extent to which increasing acidity would have on phytoplankton communities and their emission of DMSP, for deformed plankton have been observed. (Norris 2003) 3
  • 4. This would reduce the supply of nutrients that up energy back as outgoing long-wave (infrared) well from the deep. These nutrients are key for the radiation, also known as terrestrial radiation. proper functioning of phytoplankton in its euphotic Albedo is an important factor in the radiation zone. In a CLAW hypothesis reversal, this would balance, and clouds have the major effect on lead to a decline in phytoplankton activity and thus albedo. The optical properties of a cloud are a key less DMS production. If there is less DMS present issue to understanding and therefore predicting in the atmosphere there will be less cloud global climate change. A cloud's optical properties formation and so less albedo. The problem with are related to the size distribution and number of its this is that the lack of cloud cover will potentially droplets. The more cloud condensation nuclei, the lead to further climate warming. This in turn, will smaller the size of its water droplets and the higher continue to reduce the global production of DMS. the density of water droplets since the same amount of water vapor is distributed among a greater number of CCN. This affects the radiative properties (reflectance, transmittance and absorbance) of the cloud. Because of the vast amount of atmosphere between the sea and space, there is a lot of room for cloud activity. When the clouds are low and thick, they act as shields, blocking and reflecting insolation into space. This in turn cools the planet. When clouds are high up, they can also trap the outgoing heat, which is in the form of longwave radiation. This warms the planet. On the whole, data suggests that clouds have a general net cooling effect on the planet (Norris 2003). Climate scientists have realized that current models had a poor ability to accurately reproduce the effect of clouds. For this reason, scientists have made it a priority to measure and understand more about clouds physical properties and radiative fluxes. Programs like CERES, and the IRI/LDEO Climate Data Library are observing clouds from space in order to more accurately quantify cloud properties and their respective effect on albedo. If a more accurate model of cloud physics can be expressed, scientists will be able to construct more accurate simulations of climate budget and projections of change. Based on what we have learned over the years in regard to the CLAW hypothesis, it is likely that DMS has an Having a global network of biosensors can influence on the global heat budget and the help keep scientists savvy to the changes occurring hydrological cycle due to its impact on cloud in real time. The radiation balance has a formation. In order to understand how any CLAW fundamental effect on Earth's climate. About one related feedback mechanism (positive or negative) third of the solar radiation that reaches the Earth is between the plankton population and the reflected back into space by clouds and from earth atmosphere might operate, it is vital that the surfaces, such as ice and snow. The atmosphere biological role of DMS/DMSP within the cells of absorbs some solar energy, but most of the other plankton is clarified. The reason for this is because two thirds is absorbed by the land and oceans, the biological role of DMS/DMSP in plankton is which are warmed by the sunlight (Norris 2003). inextricably tied to how the feedback between The sun's energy is converted into heat, and the biology and atmosphere may respond to land and oceans then radiate a portion of this environmental changes. It seems that an 4
  • 5. understanding of this feedback process in the There will be an onboard computer with CLAW hypothesis remains elusive (Ayers et. al. power efficient processors capable of dynamically 2007). Being able to accurately quantify the adjusting their frequencies to reduce energy amount of DMS being produced in real time all consumption. These chips will likely be akin to the across the globe will be a vital contribution to the A5 processing chips at the heart of Apple’s iPad’s climate science community. and iPhones. Because accurate location Currently, some of the most recent quantification will be necessary, the units will be research in the field has come from data contained equipped with onboard GPS chips in order to in the Global Surface Sea water DMS Database. convey precise global coordinates at any time. Simo et. Al. states that there is no quality control in The super computer used for this research the database. This was worth stressing because will be a Cray XT system. Similar systems have there doesn’t seem to be unification of the DMS been installed at several operational meteorological measurement protocol, and very few and hydrological services and leading climate intercalibration exercises have been conducted in research centers worldwide. Examples include but the last 30 years. Furthermore, a number of are not limited too, NOAA, NCAR, Korea sampling and analytical issues have been reported Meteorological Administration (KMA), Brazilian in recent years. For this reason it is important to National Institute for Space Research (INPE) and have a definitive, reliable, and long lasting network Center for Weather Forecasts and Climate Studies of instruments that provide real time analysis of the (CPTEC), Danish Meteorological Institute (DMI), DMS/DMSP sea and air measurements. This will and the U.S. Naval Oceanographic Office help to assess health of the planet based on the (NAVO). (Nyberg 2010) progression of cloud formation and earths radiation In order for the unit to be able to balance. In addition it will continue to support communicate with the central data collection server James Lovelock’s Gaia hypothesis. it will utilize very low frequency (VLF) transmission to land based towers, which will then Proposal for new research be able to route the data to a server linked to a Using modified “lab on a chip” technology super computer to analyze the collected data. The developed by CalTech (Liu et. al. 2009) to reason VLF transmissions were chosen as the effectively create a network of interconnected, transmission medium is because they are often centrally linked “microlabs” to measure levels of used in Integrated Communication Systems (ICS) DMS and DMSP in phytoplankton on a global for naval vessels and HF ground-to-air scale. The labs will be encapsulated in a specific applications. The technology will likely come from vessel designed for durability and ease of Hagenuk Marinekommunikation (HMK). The maintenance and potential retrofitting. The vessel company has provided solutions for more than 25 will also be equipped with a propulsion system, navies throughout the world who now rely on the which draws energy from solar power, tidal high level of technical expertise of HMK. Over currents, or both. The unit will not only be able to 540 systems have been delivered for all classes of run real time collection and transmission of DMS ships, including 117 submarine systems. and DMSP data, it will be able to determine the Moreover, HMK provides a full service package effects of CO2 concentrations, sunlight, grazing including feasibility studies, system engineering, zooplankton, temperature and viral lysis on the hardware and software design, production, system production, dissemination and oxidation of DMS integration and setting to work as well as and DMSP. integrated logistics combined with comprehensive In order to accomplish this, the unit will be after sales services over the whole product life equipped with several sensors, including but not cycle. Lastly, the technology that allows user limited too, a PH sensor, a thermometer, a interface with the VLF system can be a single photometer, a salt refractometer, a current speed workstation that is expandable to a networking sensor, and a heavy metal sensor. The unit will multi-console client/server configuration that, also be able to rise to the surface and extend a according to the contractor, provides sophisticated probe into the atmosphere in order to collect data automated communications support for naval regarding the concentrations of DMS/DMSP in the applications. The solutions offered by HMK air directly above a particular system. posses the reliability of a company providing for 5
  • 6. the United States navy, and the customizability one phenomenon out of the trillions that exist on necessary for such a specific application. this planet, it is a step in the right direction. The communication ability of the units will boast two way transmission capabilities for References the obvious purpose of relaying collected information back to the server, and the less "Hagenuk Marinekommunikation - Naval VLF and SHF Radio obvious ability to receive remote course and Equipment." Naval Technology. Hagenuk Marinekommunikation. Web. 12 Dec. 2011.<http://www.naval- speed commands from a controlling computer. technology.com/contractors/navigation/hagenuk/>. This system would ideally be composed of several hundred of these units to create a global Greg p. Ayers, Jill M. Cainey (2007) “The CLAW hypothesis: a review of network. Ideally a climate scientist would be the major developments”, Research Front, 4, 366-374 able to identify one singular, or several units in Lana, A, G Bell, R Simo, M Vallina, and L Bopp 2011"An updated one of the many strategically placed locations climatology of surface dimethlysulfide concentrations and and have full control over the device(s). This emission fluxes in the global ocean” Global Biogeochemical will allow for a level of accurate, real time Cycles. 25. 1-17. climatic data collection never before achieved. Lovelock, James (2007). The Revenge of Gaia. Penguin. The reason each unit has its own ISBN 0141025972. propulsion system, whether it be a set of Mike Liu et. al. (2009) “Field Operational Sensor and Lab-on-a-Chip propellers or a series of pumps and jets is so the System for Marine Environmental Monitoring and Analysis” units can maintain one fixed position in the sea, CENS 1-3 or move about the sea for however long a certain Norris, Katina B. "Dimethylsulfide Emission: Climate Control by Marine experiment or research project dictates. Algae." CSA. ProQuest, Nov. 2003. Web. 12 Dec. 2011. An example of the novel application of <http://www.csa.com/discoveryguides/dimethyl/overview.php>. this technology is the fact that so far there is no Per Nyberg (2010) “Cray Supercomputers in Climate”, Weather and system of interconnected, un-tethered, real time Ocean Modeling Cray 1-6 data collecting mechanisms of this scale. There Peter M. Cox, Richard A. Betts, Chris D. Jones, Steven A. Spall, & Ian J. have been global collaborations of many Totterdell (2000) “Acceleration of global warming due to different scientists and instrumental records, but carbon-cycle feedbacks in a coupled climate model” Nature, 408, 184-187 the ingenuity behind this concept is to have one place for scientists to go to analyze the real time R. J. Charlson, J. E. Lovelock, M. O. Andreae & S. G. Warren (1987) data of the DMS/DMSP concentrations and a “Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate”, Nature, 326: 655-661 other measurable factors in the marine climate system. The information can easily be archived Rory Spowers (2000) “Interview: Living Planet” Geographical 25-27 and made public for all scientists and individuals S.M. Vallina, R. Simo, S. Gasso, C. de Boyer-Montegut et. al. (2007) who may not have the means to get to the “Analysis of a potential “solar radiation dose-dimethylsulfide- supercomputer that all the units are linked to. cloud condensation nuclei” link from globally mapped seasonal correlations” Global Biogeochemical Cycles, 21, 1-16 Furthermore, the main goal of this global network is to have the ability to monitor the Vallina, M, and R Simo. "What controls CCN seasonality in the Southern health of the planet. The possibility of the Ocean? A statistical analysis based on satellite-derived chlorophyll and CCN and model-estimated OH radical and oceanic feedback loop reversing and creating rainfall." Global Biogeochemical Cycles. 20. 1-13. another system that subjects this planet to unnecessary temperature increases is very real. James Lovelock is not the only scientist who is concerned with the future of our climate system. Although any scientist knows that the planet will survive long after humans are extinct, the focus of preventing climate change is to ensure the prosperity of humans and all other organic life alike. It is not farfetched that at some point the earth may shrug humans off its proverbial shoulder. This is why this proposal is so important. Although it is serving to quantify but 6